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VOL. 100 • NO. 10 • OCT 2019 A in the Geoscience Classrooms Leap Ahead Warming Forest Streams 100 YEARS What Happens When Subduction Stops? AGU Celebrates the Members Who Participated in 2019 Congressional Visits.

ABIGALE WYATT • ALEXANDRA KARAMBELAS • ALEXANDRA PHILLIPS • AMY HUDSON • AMY KEESEE • AMY TOWNSEND-SMALL • ANASTASIA MONTGOMERY • ANDREW MARTINEZ • ANDREW ROBISON • ANNA SCOTT • ANNALISE BLUM • ANNIE TAMALA- VAGE • BEN ABBOTT • BEN ZAITCHIK • BENJAMIN FELZER • BENNETT BEARDEN • BRAM STONE • BRENDAN KELLY • BRITTA VOSS • BRONTE • CAITLIN GRADY • CANDISE HENRY • CAROLINE DUNCAN • CAROLINE LADLOW • CAROLYN ROBERTS • CHERYL MANNING • CHRISTINE KIRCHHOFF • CHRISTINE SHIELDS • JACKSON • DANIEL ZISKIN • DAVID GORELICK • DAVID HASTINGS • DAVID HEATH • DAVID KAHLER • DAVID TROSSMAN • DEAN MOOSAVI • DENISE HILLS • DIANA ZAMORA-REYES • DILLON AMAYA • DINA ABDEL-FATTAH • DIVYA SAXENA • DORK SA- HAGIAN • ELIZABETH HETHERINGTON • EMILIE SINKLER • EMILY FIRST • EMILY YANG • EVELYN POWELL • LINAM • FREDERICK BLUME • GIFFORD WONG • HEIDI STELTZER • HENRY POTTER • IAN BOLLIGER • JACKIE RATNER • JACOB HAQQ-MISRA • JASON COENEN • JENNIFER BURNEY • JENNIFER SCULLY • JESSIE PEARL • JISOO KIM • JOANNA CAREY • JOHN GEISSMAN • JOHN JONES • JOHN PERRY • JOSH PAPACEK • KAMINI SINGHA • KATHERINE STRAUB • KIMBERLY DUONG • KRISTI FINK • KRISTIN TIMM • KRISTINA PISTONE • LAURA SZYMANSKI • LAUREN HOLDER • LINDSEY KEN- YON • LISA TRANEL • LOGAN • LORENE LYNN • MARC MAYES • MARLON RAMOS • MARYANN MALINCONICO • MATTHEW MEKO • MCKENZIE SKILES • MELANIE ABECASSIS • MEREDITH RICHARDSON • MEREDITH SCHERVISH • MICHAEL • MICHAEL HAMBURGER • MICHAEL HIRSCH • MICHAEL O’CONNOR • MICHELLE TIG- CHELAAR • MIKE MADDEN • MITCH ROFFER • MOLLY • NIKKI SEYMOUR • PAUL SZEJNER • PERRI SILVERHART • RACE • RACHEL HOHN • RACHEL OWEN • REBECCA WARD • REINALDO ALCALDE • RYAN HAUPT • RYAN THALMAN • SEAN HEUSER • SHAINA ROGSTAD • SHIMA BAHRAMVASH SHAMS • SINGLETON THIBODEAUX-YOST • SKYLER MAVOR • SOUMAYA BELMECHERI • STEPH COURTNEY • STEWART WILLIAMS • SUSAN BATES • SUSAN KASPARI • SUSAN NOSSAL • TAI-YIN HUANG • TESSA HILL • TIM MELBOURNE • VICKI MCCONNELL • VICTORIA KEENER • VIRGINIA MARCON • WILLIAM LANDING • ZACHERY LIFTON FROM THE EDITOR

Editor in Chief Heather Goss, AGU, Washington, D.C., USA; [email protected]

This Is How the World Moves Editorial Manager, News and Features Editor Caryl-Sue Micalizio Science Editor Timothy Oleson t didn’t exactly crack open the world, the around this time, and Senior News Writer Randy Showstack presentation Princeton University’s Jason then, about 5 million News Writer and Production Associate Kimberly M. S. Cartier I Morgan gave at AGU’s Spring Meeting in years ago, the sub- News and Production Fellow Jenessa Duncombe Washington, D.C., in April 1967. However, duction underneath Morgan’s research leading up to the meeting Sabah just…stopped. Production & Design had proved that there were, in fact, cracks in The scientists, as Manager, Production and Operations Faith A. Ishii Senior Production Specialist the world. they write, want “to Melissa A. Tribur Editorial and Production Coordinator Liz Castenson “It seems extraordinary that, in this hall understand why sub- Assistant Director, Design & Branding Beth Bagley packed with the best geophysicists and geolo- duction ceased and Senior Graphic Designer Valerie Friedman gists in the , nobody got excited how the of Graphic Designer J. Henry Pereira or even interested by the implications of Mor- Sabah may be related gan’s ideas. They were too new, too different to deeper processes in the .” Read more Marketing from anything which had been done,” wrote about their work and the seismic network Director, Marketing, Branding & Advertising Jessica Latterman Assistant Director, Marketing & Advertising Xavier Le Pichon in the journal Tectonophysics they’ve installed on page 18. Liz Zipse Marketing Program Manager Angelo Bouselli in 1990, when he aimed to “reconstruct what Some of our biggest questions about tecton- Senior Specialist, Digital Marketing Nathaniel Janick happened during those exciting six months.” ics and seismic hazards could be answered if Digital Marketing Coordinator Ashwini Yelamanchili Morgan had, of course, proved the theory of scientists could better understand the plate through Peninsula subduction zone. On page 30, read Advertising measurements. “The evidence presented here about a large group of researchers who Display Advertising Dan Nicholas [email protected] favors the existence of large ‘rigid’ blocks of launched the Alaska Amphibious Community Recruitment Advertising Heather Cain ” that explained , he Seismic Experiment in May 2018, deploying a [email protected] wrote in the conclusion of his landmark paper, huge array of seismometers that stretch from “Rises, , great faults, and crustal onshore far out into the , using innova- Science Advisers blocks,” published in March 1968 in AGU’s tive bottom seismometers that work Geomagnetism, Paleomagnetism, Julie Bowles and Electromagnetism Journal of Geophysical Research. (Morgan’s together to take integrated observations. The Space Physics and Aeronomy Christina M. S. Cohen paper, held up in peer review, came several researchers collected their instruments in Study of the ’s Deep Interior Edward J. Garnero months after Nature published similar results August and are making the data freely avail- Geodesy Brian C. Gunter from Dan McKenzie and Robert Parker, who able as quickly as they are recovered. History of Kristine C. Harper Planetary Sciences Sarah M. Hörst were largely credited as the first scientists to What’s next for the field of tectonics? We Natural Hazards Michelle Hummel verify . Le Pichon eventually might ask Jacqueline Austermann of Columbia Volcanology, , and Petrology Emily R. Johnson found a copy of the outline Morgan had scram- University. AGU’s Tectonophysics section Keith D. Koper bled to finish the night before his 1967 talk— recently honored her with its Jason Morgan Tectonophysics Jian Lin Near-Surface Geophysics Juan Lorenzo neither Morgan nor several colleagues had Early Career Award. Our hearty congratula- Earth and Space Science Informatics Kirk Martinez retained their copies. The document showed tions go to all the 2019 section awardees and and Figen Mekik that Morgan should be credited for the feat.) named lecturers, as well as to AGU’s Union Mineral and Rock Physics Sébastien Merkel For AGU’s Centennial, this month in Eos medal, award, and prize recipients, and, Ocean Sciences Jerry L. Miller Global Environmental Change Philip J. Rasch we’re celebrating all the scientists who have finally, the warmest of welcomes to our 2019 Education Eric M. Riggs been fascinated by the idea, since it was first class of AGU Fellows. We look forward to hon- Tectonophysics Carol A. Stein proposed by in 1912, that the oring your achievements in San Francisco at Atmospheric Sciences Mika Tosca continents shift underneath our feet, con- Fall Meeting 2019. See the announcements for Nonlinear Geophysics Adrian Tuck Earth and Processes Andrew C. Wilcox stantly reshaping the planet. all your distinguished colleagues starting on Atmospheric and Space Electricity Yoav Yair Our cover story features scientists studying page 36. GeoHealth Ben Zaitchik striking formations in . Mount Kina- With this much knowledge and passion Societal Impacts and Policy Sciences Mary Lou Zoback balu (pictured on the cover) in the Malaysian among our members, we look forward to feel- state of Sabah is a spectacular example of ing the metaphorical ground shift beneath us ©2019. AGU. All Rights Reserved. Material in this issue may be photocopied by individual scientists for research or classroom use. Permission is also granted to use plate tectonics at work. The soon once more. short quotes, fi gures, and tables for publication in scientifi c books and journals. For permission for any other uses, contact the AGU Publications Offi ce. formed when rising from the active Eos (ISSN 0096-3941) is published monthly by AGU, 2000 Florida Ave., NW, subduction zone below squeezed between two Washington, DC 20009, USA. Periodical Class postage paid at Washington, D.C., rock strata and then cooled rapidly—because and at additional mailing offi ces. POSTMASTER: Send address changes to Member Service Center, 2000 Florida Ave., NW, Washington, DC 20009, USA of mechanisms still not entirely understood— Member Service Center: 8:00 a.m.–6:00 p.m. Eastern time; Tel: +1-202-462-6900; about 7 million years ago. Several other Fax: +1-202-328-0566; Tel. orders in U.S.: 1-800-966-2481; [email protected].

strange landforms nearby were also created Heather Goss, Editor in Chief Submit your article proposal or suggest a news story to Eos at bit.ly/Eos-proposal. Views expressed in this publication do not necessarily refl ect offi cial positions of AGU unless expressly stated. Christine W. McEntee, Executive Director/CEO

Earth & Space Science News Eos.org // 1 CONTENTS

24

30 Features

24 John Wesley Powell 18 and the West That Wasn’t Cover Story By Korena Di Roma Howley

One hundred fifty years ago, the explorer and scientist argued that the West needed smart 18 The Fate of Borneo’s development. Now the ­fast growing region is Plunging Tectonic Plates playing catch-­ up.​­ By Simone Pilia et al.

Scientists installed a dense seismic network to investigate what 30 Understanding happens when subduction stops. Alaska’s By G. A. Abers et al. On the Cover One of the longest deployments of new Mount Kinabalu in the Malaysian state of Sabah in northern Borneo. seafloor seismograph technology was just Credit: rmnunes/Depositphotos.com completed—and you can get the data now.

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12 40 Columns

From the Editor AGU News

1 This Is How the World Moves 36 2019 AGU Section Awardees and Named Lecturers 38 2019 Class of AGU Fellows Announced News 39 2019 AGU Union Medal, Award, and Prize Recipients Announced 4 Majority of YouTube Videos Promote Nonconsensus Views 5 The Dawning of the Age of Old Aquifers Research Spotlight 6 Paleontologists Peer Inside Billion-Year-Old Cells 40 Forested Streams May Warm More Than Observations 7 Wind-Triggered Ground Shaking Masks Microseismicity Predict 8 Nearest Star System May Have a Second Planet 41 Variations in Creep Along One of Earth’s 9 Murders of Environmentalists Have Doubled in 15 Years Most Active Faults 11 Earthquakes Shake Up Systems 41 A Better Way to Measure Cloud Composition 12 First Persian Gulf Meteotsunami Spotted 42 New Perspectives on 2,000 Years of North Atlantic Climate Change Opinion 43 Déjà Vu: Understanding Subduction Zones’ Cycle of Seismicity 13 Uncontrolled Chemical Releases: A Silent, 43 Demystifying Level Changes Along Growing Threat the New England Coast 15 An Evolutionary Leap in How We Teach Geosciences Positions Available

44 Current job openings in the Earth and space sciences Postcards from the Field

48 The Investigation of Seismicity in Louisiana project team earns a rainbow for their hard work.

AmericanGeophysicalUnion @AGU_Eos company/american-geophysical-union AGUvideos americangeophysicalunion americangeophysicalunion

Earth & Space Science News Eos.org // 3 NEWS

manipulation” (75%), “climate modification” Majority of YouTube Climate Videos (95%), and “geoengineering” (90%) and also appeared in other search results. Promote Nonconsensus Views People searching for information on climate mitigation strategies “won’t find any informa- tion on these topics in the way they are dis- cussed by scientists and engineers,” Allgaier concluded. “Instead, searching for these terms results in videos that leave users exposed to entirely ­non-​­scientific video content.” When it comes to numbers of views, climate consensus videos (not including debates) hold a slight edge over the nonconsensus and con- spiracy videos: about 2,300 more views out of more than 34 million.

Taking Climate Videos Because YouTube decides which videos appear in a search and which videos it profits from in advertising, it should play a part in the solu- tion, Allgaier argues. “I think YouTube should take responsibility to ensure its users will find high-­ ​­quality infor- mation if they search for scientific and bio- medical terms, instead of being exposed to doubtful conspiracy videos,” he said. The move would have precedent: Earlier this year, YouTube and other social media platforms removed advertising from anti-­ vaccine​­ videos

iStock.com/pressureUA and categorized them as “dangerous and harmful” content. f an average Internet user opens ­YouTube to every month. Science teachers and professors Scientists and science communicators can learn about climate change, they might use YouTube videos to enhance curricula, and a play a key role too. “YouTube has an enormous I search for “global warming” or “climate growing body of research shows that YouTube engineering” or simply “climate change.” can be a ­self-education​­ tool outside the class- What videos will show up? A new study found room. People searching for that more than half of the videos that appear But misinformation and conspiracies information on climate in ­climate-related​­ YouTube search results abound with climate science, particularly on promote views that oppose the scientific con- social media, and it’s unclear which videos mitigation strategies sensus on climate change. might appear for typical Internet users who “Searching YouTube for climate-­ science-​­ don’t normally search for science videos. “won’t find any and climate-­ engineering-​­ related​­ terms finds To answer that question, Allgaier mined information on these fewer than half of the videos represent main- YouTube using 10 common climate-­ related​­ stream scientific views,” Joachim Allgaier, a search terms—for example, “climate,” “cli- topics in the way they are senior researcher at Rheinisch-­ Westfälische​­ mate change,” “geoengineering,” “global Technische Hochschule Aachen University in warming,” and “chemtrails”—and used an discussed by scientists Germany, said in a statement in July. online anonymity network so that searches and engineers.” Fewer videos promoted outright climate would not be affected by past activity. He then change denial than those supporting the sci- evaluated the search results on whether the entific consensus, but chemtrail conspiracy videos promoted the consensus view on videos were the most numerous. “It’s alarm- ­human-induced​­ climate change from the reach as an information channel, and some of ing to find that the majority of videos propa- Intergovernmental Panel on Climate Change. the popular science YouTubers are doing an gate conspiracy theories about climate science Of the 200 ­climate-related​­ videos he ana- excellent job at communicating complex sub- and technology,” he said. lyzed, Allgaier found that 44.5% promoted the jects and reaching new audiences,” Allgaier Overall, climate consensus videos were scientific consensus view and a further 2% said. “Scientists could form alliances with sci- slightly more popular than nonconsensus vid- were in a debate format that also included ence communicators, politicians, and those in eos. The study was published on 25 July in Fron- nonconsensus views. Only 8% of the videos popular culture in order to reach out to the­ tiers in Communication (bit.ly/youtube​­ -​ science).­ focused on outright climate change denial. widest possible audience.” The remaining 45.5% of videos focused on A Powerful (Mis)information Platform climate conspiracy theories about chemtrails. YouTube reports that nearly 2 billion ­logged-​ Chemtrail conspiracy videos dominated search By Kimberly M. S. Cartier (@AstroKimCartier), ­in users around the world access its platform results for “chemtrails” (95%), “climate Staff Writer

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In the Negev, Yokochi said, there is cur- The Dawning of the Age rently no occurring. But in the geologic past, the area went through of Old Aquifers climate changes, including wetter conditions that renewed the aquifers. Yokochi said that previous work in the Negev used carbon-­­ 14​­ (14C) to date groundwa- s water moves from high in the sky to sandstone aquifer. They note that their ter reserves to about 30,000 years. The prob- deep in the ground, it picks up chemi- method can be used to reconstruct paleocli- lem with using 14C is that the isotope extends A cal signatures that can tell researchers mates from aquifers around the globe. back in time only 30,000–­­ 40,000​­​­​­ years, secrets about Earth, from the density of air meaning that the age of older water remained pollution to global ice cover to what kind of Arid Aquifers a mystery. rock the raindrops seeped through. Scientists Groundwater is an important resource for Using the noble gas isotope 81Kr solved can look at specific radioactive isotopes and on the planet, especially in arid regions. this problem. ­­Krypton-81​­ is found through- reconstruct past and weather pat- Replenishing, or recharging, groundwater out the troposphere, where it mixes with terns recorded in stored groundwater. requires that rainfall soak into the soil, travel- raindrops. In a paper published in August in the Pro- ing downward for storage in aquifers—a pro- “Once that water is isolated from the atmo- ceedings of the National Academy of Sciences cess that requires recurring wet periods. sphere [in the ground], there’s no more sup- of the United States of America (bit.​ ly/­ pnas​­­ ​ “Groundwater can serve as a paleo-­­ ​ ply, and it decays,” Yokochi explained. “That’s -aquifer),­ researchers leveraged an isotope of ­humidity, -​­precipitation proxy,” said Reika when the clock starts.” krypton (Kr) that can reach more than a mil- Yokochi, a geochemist at the University of Yokochi said that 81Kr, with its ­­half-​­life of lion years back in time to discover the age of Chicago and lead author of the paper. By using about 230,000 years, allowed the team to mea- groundwater in the Negev desert in Israel. groundwater as a record of past climate condi- sure the age of aquifers that are up to 1.3 mil- Pairing krypton with other isotopes in tions, researchers can use that information to lion years old—a huge extension from 14C. groundwater, the researchers found two dis- better predict how precipitation might change “Krypton isotope dating of groundwater is tinct ages and sources within the Nubian in the future. exciting, as it opens a new window into past

The aquifer beneath the arid Negev desert in southern Israel is no longer being recharged but once was fed by sources from the Mediterranean and the Atlantic. Credit: Mark A. Wilson, CC0 1.0 (bit​.­ly/​ccby1-0)

Earth & Space Science News Eos.org // 5 NEWS

climatic conditions that was previously unavailable, or cloudy, with existing dating Paleontologists Peer Inside techniques,” said Jennifer McIntosh, a hydro- geochemist at the University of Arizona not ­Billion-​­Year-​­Old Cells involved in the research. “This is one of the few studies to use groundwater as a record of paleoclimate beyond the Last Glacial Maximum,” said cotland contains an amazing array of McIntosh. wildlife: Puffins, Scottish wildcats, and S orcas all make northern Great Britain Aging an Aquifer their home. But paleontologist Eva Sirantoine Yokochi said that in the past, amassing and her colleagues weren’t looking for any of enough krypton gas in a water sample required these animals; the creatures they were inter- sampling about ­­200–300 liters. Bringing that ested in were much, much smaller. They had much water back to a lab for analysis is “a lot also been dead for nearly 1 billion years. to carry,” so Yokochi said that she and her The picturesque sandstone outcroppings of team used a field gas extraction device. northwestern Scotland’s Cailleach Head For- The team used atom trap trace analysis mation are studded with tiny gray phosphate (ATTA) methods to measure krypton isotopes nodules. To the casual observer, they might in the lab. The combination of field gas not look particularly special, but in fact, they extraction and ATTA bolstered the team’s contain exquisitely preserved microfossils of The gray phosphate nodules in this sandstone contain ability to collect water from 22 wells in the Precambrian cells. microfossils of Precambrian organisms. Credit: Eva eastern Negev. In a recent study published in Scientific ­Sirantoine “Everything became more efficient and Reports, scientists from the University of fast,” said Yokochi. Western Australia and Boston College report The researchers found that 81Kr data revealed that they were actually able to peer inside appears to be eukaryotic (a more complex cell two distinct groundwater recharge dates: one these ancient cells (bit.​ ly/­ cells­ -​ preserved).­ type that has a nucleus, like animal and plant less than 38,000 years ago and a much older Sirantoine said that by using scanning trans- cells). These fossilized cells were once part of wet period about 360,000 years ago. mission electron microscopy combined with a an ancient lake ecosystem. Pairing this information with hydrogen technique called energy dispersive spectros- and oxygen isotope data from the samples, copy, the team was able to get an idea of the Preserved by Rare Earth Elements the team found that the younger aquifer was The researchers think that the cells actively recharged with water sources from the Medi- absorbed and retained the rare earth element terranean, whereas the older wet period “That’s what I think is (REE) phosphates monazite and xenotime. brought precipitation from the tropical cool about this study—it When the cells died, these REE phosphates ­Atlantic. precipitated rapidly, preserving the inner “Knowing the source of the water helps sci- opens up this new search workings of the cells. entists understand past climatic conditions Sirantoine said that ancient microfossils that led to groundwater recharge and how vul- image, this new place to can help us understand when and where nerable the aquifer is to future climate go look and quest for eukaryotic cells developed and diversified, change,” said McIntosh. “This information which was a major step in the evolution of life can be used to inform paleoclimate models other preserved fossils.” on Earth. and aid in water management decisions.” Alison Olcott Marshall, a paleobiogeochem- Other studies have used 81Kr as a tracer, but ist at the University of Kansas who was not Yokochi said that “this is the first case where involved in the study, said that this is an we take a lot of data from a very small area, do ­three-dimensional​­ structure of the fossilized exciting finding. “The farther you go back in the spatial distribution analysis, and talk cells as well as to obtain information about the time, the fewer rock units there are that are about climate.” chemical composition of specific regions likely to preserve signs of life.… So we all tend McIntosh said she anticipates—and is within them. to cluster in the same units because there’s excited for—krypton isotopes to be widely Sirantoine said that microfossils like these only a limited number of targets. As scientists, used in future studies. provide us with a window into the distant we have a sort of search image for what kinds “Knowing how ‘old’ groundwater is helps past. “Most fossils are not as good, so it’s like of rocks are good targets. These [samples from water managers evaluate how much water having a bad camera with a bad lens: You get a the present study] are rocks that wouldn’t they can extract without significantly deplet- blurred image, so you can’t really tell what’s in necessarily have been somebody’s first place ing the aquifer,” said McIntosh. “It can also the picture. But when you get very nice fossil to think of to look. So that’s what I think is help them determine how vulnerable the deposits like this one, you have a much cool about this study—it opens up this new aquifer is to anthropogenic sources of con- sharper picture. Studying this ­well-preserved​­ search image, this new place to go look and tamination.” deposit gives you a better picture of what the quest for other preserved fossils.” diversity was like.” This group of billion-­ year-​­ old​­ microfossils By Sarah Derouin (@Sarah_Derouin), Freelance­ contains what appear to be prokaryotic cells By Hannah Thomasy (@hannahthomasy), Journalist­ (cells without a nucleus) and one cell that ­Freelance Science Writer

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Wind- Triggered Ground Shaking Masks Microseismicity

he earthquakes that jolt us out of bed, how one the ones that trigger an instinctual urge triggers others. T to duck and cover, are powerful and To test how ground potentially destructive. shaking was cor- But they’re also rare: For every magnitude related with wind 7.0 temblor, roughly a million magnitude 1.0 strength, the scien- earthquakes occur. tists also measured Earthquake detection algorithms must be wind velocity using able to accurately disentangle these numer- an anemometer ous, low- amplitude seismic signals from other mounted near the sources of ground shaking such as aircraft ranch’s unused air- passing overhead and waves crashing into strip. They recorded coastlines. Now researchers have analyzed the an average wind waveforms of wind- induced ground motion, velocity of roughly work that will boost the performance of future 2 meters per second earthquake detection algorithms, the scien- and a maximum wind tists suggest. velocity of about 15 meters per second. Research on a Ranch Masquerading Christopher Johnson, a seismologist at the Researchers studied wind- induced ground movement near Anza, Calif. Credit: Christo- as an Earthquake Scripps Institution of in San pher Johnson Diego, Calif., and his colleagues collected data Johnson and his col- on a privately owned unused ranch situated laborators found that atop the San Jacinto zone near Anza, gusts of wind stron- Calif. Johnson and his team placed 40 geo- ger than a few meters per second were linked Shaking Deep Down, Too phones around the property’s stands of vege- to ground shaking characterized by earth- The scientists recorded wind- induced tation, old structures, abandoned machinery, quake like waveforms. The team examined the ground motion not only in the geophones and defunct airstrip. The coffee can– sized vertical and horizontal components of the resting on the ground but also in a 148- instruments, anchored to the ground with a wind-triggered shaking and found a consis- meter borehole that had been previously roughly 12- centimeter- long metal spike, tently larger signal in the horizontal direction. drilled and instrumented with a seismome- recorded ground velocity measurements 500 That’s because the wind is pushing abo- ter. times per second from 9 February through veground objects—like structures, vegetation, “We can see that [the wind energy] is going 17 March 2018. and machinery—with a shearing motion with into the ground,” said Johnson. He and his The scientists wanted to better understand respect to the ground, said Johnson. colleagues published their findings in July in ground movement caused by wind energy Next, the researchers investigated the the Journal of Geophysical Research: Solid Earth being transferred into Earth through, for strength of the wind- triggered shaking at dif- (bit.ly/ ground - motion). example, plant roots or building foundations. ferent locations on the ranch. They recorded These results are important, said Adam That’s important, researchers said, because the weakest signal on a hill and the strongest Ringler, a geophysicist with the U.S. Geologi- wind- induced ground shaking, which affects signal near a covered parking structure. These cal Survey at the Albuquerque Seismological roughly the top kilometer of Earth’s crust, is a results make sense, said Johnson, because Laboratory on Kirtland Air Force Base, N.M., source of noise in seismic records. human- built structures are coupled to the not involved in the study. “By improving our “We need to have a really good understand- ground through their foundations, which understanding of how nonearthquake signals ing of what all of these noise signals are,” said means that wind energy is efficiently trans- get recorded by sensors, we can improve our Johnson. ferred into the ground. ability to detect small events and characterize Seismic records are increasingly being mined The scientists also found that wind- induced them.” to find new fault lines and better understand ground movement was sometimes strong In the future, Johnson and his team want to enough to mask seismic signals arising from place more geophones near the San Jacinto “We need to have a really slipping faults. “About 6% of the day, there fault zone. “We’ve been focusing on small are wind- induced ground motions with ampli- areas, but you could imagine putting them out good understanding of tudes greater than what we’re anticipating for over 20 kilometers,” said Johnson. “They’re microseismicity,” said Johnson. That’s bad quick and easy to deploy.” what all of these noise news because much can be learned from these signals are.” tiny earthquakes. “These tell a lot about the dynamics of fault zones and foreshock and By Katherine Kornei (@katherinekornei), aftershock sequences.” Freelance Science Journalist

Earth & Space Science News Eos.org // 7 NEWS

of the host star, which showed a characteristic Nearest Star System wobble from the planet’s gravitational influ- ence. Damasso and his team sought to validate May Have a Second Planet Proxima b’s existence by analyzing the same data using a different method. They took par- ticular care when accounting for Proxima’s stellar flares and spots. “Stellar activity can hamper the radial velocity [analysis] because there can easily be present some signal from the stellar activity in the data,” Damasso said. After accounting for Proxima’s stellar activity and Proxima b’s radial velocity signal, the team noticed a periodic signal left over in the data. That signal suggested that a second planet was tugging on Proxima. To make the signal, a planet would need to be at least 6 times Earth’s mass and orbit at about the same distance as Mars is from the Sun. “This detection is quite challenging, partic- ularly because it’s made with only one tech- nique,” Damasso said. “And the orbital period is very long, so it takes a long time to collect more data.” “Is this planet habitable? Well, not really. It’s quite cold,” said team member Fabio Del Sordo, an astrophysicist at the University of Crete in Greece. “We estimated a surface equi- librium temperature of only 40 kelvins,” which is −233°C. “So, clearly not habitable.”

A Long Road to Confirmation At the April forum, University of Hawai‘i astronomer Lauren Weiss voiced concerns that a second Proxima planet might not be where or what the team thinks it is. “In any system, you don’t know what plan- ets there are [that] you haven’t found yet until you find them,” Weiss said. “They are an unknown unknown, which makes it very chal- lenging to accurately model and fit radial velocities.” She explained that the signal attributed to Proxima c could very well be a combination of other, weaker signals. “That maybe means An artist’s impression of Proxima b in orbit around the flaring red dwarf star Proxima Centauri, with two other stars in that there are additional planets but not at the the background. Scientists suspect that there is also a larger, colder planet in this solar system. Credit: Ricardo period at which [they’re] announcing the can- Ramirez and James Jenkins, Department of Astronomy, Universidad de Chile didate,” she said. Weiss recently told Eos, “I have seen no additional data supporting or falsifying the n 2016, astronomers announced the discov- If confirmed, this planet would make Prox- proposed orbit and minimum mass of the ery of a rocky, habitable, ­­Earth-sized​­ planet ima Centauri our nearest multiplanet system planet candidate Proxima Cen c” since the ini- I orbiting Proxima Centauri, the closest star and challenge our understanding of how rocky tial announcement in April. beyond our solar system. A recent analysis planets larger than Earth form. Damasso dis- With its currently calculated orbit, Prox- now suggests that Proxima might also host a cussed Proxima c on 19 August at the Extreme ima c would challenge our understanding of larger, colder planet. Solar Systems IV conference in Reykjavík, Ice- how planets that size form, Del Sordo said. “We call it Proxima c,” Mario Damasso, an land. This discovery is currently under peer “Since ­­low-mass​­ stars are expected to host astrophysicist at the Astrophysical Observa- review in Science Advances. multiplanet low-­­ mass​­ systems, Proxima could tory in Torino, Italy, said about the potential certainly host other terrestrial planets we discovery at a forum in April. “But it’s only a Bigger, Colder, Farther Away could not detect,” Damasso told Eos about his candidate. That’s very important to under- Astronomers found the 2016 planet, Prox- presentation in Iceland. “Analyzing the avail- line.” ima b, using radial velocity (RV) measurements able RV data with methods different from that

8 // Eos October 2019 NEWS

Murders of Environmentalists Have Doubled in 15 Years

nvironmental activists and defenders from the international environmental orga­ are killed at twice the rate that they were nization Global Witness (bit.ly/​ chain​­ -​ of­ ​ E 15 years ago, according to a new study. -violence).­ Researchers found that more environmental The researchers found that 1,558 people in defenders were murdered in countries with a 50 countries around the world were killed weaker rule of law and where more land area defending the environment between 2002 and was harvested. 2017. “This is more than double the number of “Environmental defenders help protect and Australian armed service land, forests, water and other natural people killed on active duty in war zones over resources,” Nathalie Butt, lead author of the the same period…and almost half as many as study, said in a statement. “They can be any- the number of U.S. soldiers killed in Iraq and one—community activists, lawyers, journal- Afghanistan since 2001,” the study says. ists, members of social movements, [nongov- During those 15 years, the rate at which ernmental organization] staff, and indigenous environmental activists were murdered people—anyone who resists violence.” increased from two murders per week to four “As consumers in wealthy countries—who per week. The death toll in Brazil, the Philip- are effectively outsourcing our resource con- pines, , and Honduras represented sumption—we share responsibility for what’s about 71% of all environmentalists killed happening,” said Butt, who studies the eco- during that time period. logical impacts of climate change at the Uni- One particularly concerning finding is that versity of Queensland in St. Lucia, Australia. about 40% of the murders in 2015 and 2016, “Businesses, investors, and national govern- and about 30% of the killings in 2017, were of Proxima Centauri is only slightly larger than Jupiter and is ments at both ends of the chain of violence indigenous persons. More indigenous people much smaller, cooler, and dimmer than the other two stars need to be more accountable.” were killed defending their land and environ- in that system (Alpha Centauri A and B). Credit: European ment than were people of any other group. Southern Observatory, CC BY 4.0 (bit.ly/ccby4-0)​­ Environmentalists Dying “This is a phenomenon seen around the Around the World world: land and environmental defenders are The study, which was published in Nature Sus- declared terrorists, locked up or hit with para- we used could reveal additional signals worthy tainability on 5 August, analyzes reports of lyzing legal attacks, for defending their rights, of attention.” environmentalists’ deaths around the world or simply for living on lands that are coveted “Models tell us that super-­­ ​­ tend to form around the snow line, but Proxima c at the moment is quite distant from the snow line,” he said. “It’s possible that this planet migrated from somewhere else in the sys- tem.” “We plan to go on with radial velocity ­­follow-up”​­ as well as direct imaging with ground-­­ based​­ instruments, Damasso said. “This is a necessary step to do since the orbital period of the candidate is [about] 5 years long.” And with future astrometry data from the European Space Agency’s Gaia mission, “we should be able to measure the mass with 5% accuracy, which is great news for us,” Del Sordo said. “This will take place in a couple of years with the end-­­ of-​­ mission​­ data.” When it comes to confirming Proxima c’s existence, “it’s going to be a long road,” Weiss said. Munduruku people hold signs with slogans like “Dam Kills!” during a protest of the Belo Monte hydroelectric dam in Brasilia, Brazil, in 2013. Munduruku and other indigenous Brazilian people argue that the dam will disrupt their way of By Kimberly M. S. Cartier (@AstroKimCartier), living through deforestation and flooding and protested attacks against and murders of natives. Credit: EVARISTO SA/ Staff Writer AFP/Getty Images

Earth & Space Science News Eos.org // 9 NEWS

Researchers found that more environmentalists were killed (larger circles) in countries with lower rule of law (ROL) scores (lighter blue). Credit: Nathalie Butt

by others,” stated Victoria ­Tauli-Corpuz,​­ the an overall conviction rate of 43% in 2012, but United Nations Special Rapporteur on the the conviction rate was only 10% for the kill- “Corruption was the key rights of indigenous peoples. ings of environmentalists. correlate for the killings.” “Although conflict over natural resources is Killing for Natural Resources the underlying cause of the violence, spatial and Getting Away with It analyses showed corruption was the key cor- The researchers also gathered data from relate for the killings,” Butt said. “In many in the number of deaths related to water ­organizations that track rule of law and instances, weak rule of law means that cases resources. The 2018 report was released days environment-­­ related​­ business sectors. They in many countries are not properly investi- before unrelated reports from the World found that the mining, agribusiness, water gated, and sometimes it’s the police or the Resources Institute on global water stress and resources, and logging sectors were tied to or authorities themselves that are responsible from the Intergovernmental Panel on Climate suspected in the highest number of deaths. for the violence.” Change on vulnerabilities in the land and More deaths occurred in countries with higher food sectors. corruption rates and a weaker rule of law. Criminalizing Environmental Activism Last year, Global Witness also tracked a rise What’s more, murders of environmentalists Global Witness released its 2018 report on in the criminalization of activism, including in were much less likely to have legal ramifica- attacks against environmental defenders on the United Kingdom and Iran, a trend that the tions than were other murders: Homicides had 30 July (bit.​ ly/­ gw​­ -​ attack­ -​ stats).­ The organiza- agency says has continued so far in 2019. The tion found that 164 organization specifically called out Brazilian people were killed president Jair Bolsonaro and U.S. president last year, an average Donald Trump for agendas that promote busi- rate of more than ness over the environment and for policies three per week. that strip away environmental and human “Countless more rights protections. were silenced “It is a brutal irony that while judicial sys- through other tactics tems routinely allow the killers of defenders to designed to crush walk free, they are also being used to brand protest, such as the activists themselves as terrorists, spies or arrests, death dangerous criminals,” Alice Harrison, a senior threats, lawsuits and campaigner at Global Witness, said in the smear campaigns,” statement accompanying the report. “Both the agency stated. tactics send a clear message to other activists: Mining and agri- the stakes for defending their rights are pun- business remained ishingly high for them, their families and their the first-­­ and communities.” On 22 May 2018, roughly 20,000 environmental protesters marched toward a Sterlite Cop- second-­ deadliest​­ per mining plant in Tamil Nadu in southern . The plant was linked to soil, water, and air sectors for environ- pollution in the area. State police killed 13 protesters in what was the largest massacre of mentalists, but last By Kimberly M. S. Cartier (@AstroKimCartier), environmental defenders in 2018. Credit: Mksr2020, CC ­­BY-SA 4.0 (bit.ly/​ccbysa4-0) year also saw a spike Staff Writer

10 // Eos October 2019 NEWS

Earthquakes Shake Up Groundwater Systems

fter an earthquake, regional stream- flows will sometimes increase because A of an influx of groundwater being released from aquifers. This phenomenon is well documented, but the details of the under- lying mechanisms remain somewhat mysteri- ous. A new study looking at the effect of the 2011 Tohoku earthquake in Japan on groundwater systems in China is shedding some light on how Earth’s subsurface can be affected by large earthquakes. Groundwater systems often comprise layers of permeable rock called aquifers separated by low- permeability layers called aquitards. Pre- vious studies have analyzed the effects of earthquakes on either aquifers or aquitards, but to date, nobody has quantified the effects of earthquakes on both aquifers and aquitards in the same groundwater system, said Zhe- ming Shi, a hydrogeologist at the China Uni- versity of Geosciences in Beijing and an author of a study published in May in (bit.ly/ wrr- groundwater - system). Earthquakes like the 2011 Tohoku earthquake in Japan can wreak havoc on local infrastructure like this, as well as “The commonly used tidal response models increase the permeability of aquifers thousands of kilometers away. Credit: iStock. com/ egadolfo can only identify either aquifer or aquitard permeability, not both at the same time,” Shi said. study. Manga coauthored a commentary about settled after the Tohoku event, detectable Shi and colleagues took a different approach, the study’s findings in June in Water Resources changes in the well returned to preseismic combining a traditional tidal response model Research along with Steve Ingebritsen, a levels in about 4 months, Shi and his col- with an analysis of barometric pressure hydrologist with the U.S. Geological Survey leagues wrote. changes detected in a 2,600- meter- deep well (bit. ly/ wrr - hydrologic - responses). “This is a very clever study that’s adding a near the Shunyi- Qianmen- Liangxiang fault “Permeability is not usually thought of as a lot to this discussion of how permeability can zone, one of the largest fault systems in Bei- quantity that can change over time,” Manga change in space and time,” Ingebritsen said. jing. said. “When you drill a well, you measure the “I think there’s growing interest in this idea Scientists have been monitoring subsurface rate of flow and then that’s the number you that permeability is a mutable property. I’d changes in this well—drilled into an aquifer in use” to describe the productivity of that well. like to see more of these kinds of studies porous that is capped by layers of But during an earthquake, subsurface pres- done in other wells in other geologic set- impermeable mudstone, sandstone, and sure changes, and new fracture networks and tings.” —for decades as part of the country’s shifting gases and fluids can open new path- The work may also have implications for extensive earthquake monitoring program. By ways for groundwater movement. The new groundwater quality after an earthquake, Shi comparing barometric pressures recorded study also demonstrates that these subsur- said. Increases in the aquitard’s permeability 4 months before the 11 March 2011 Tohoku face shifts are not permanent: As the area may allow pollutants to find their way into quake with data collected up to a year after the groundwater supplies. event, they found that the earthquake boosted “The aquitard is a good indicator of the the permeability of the aquifer by a factor of 6, A new study looks at the aquifer’s vulnerability to pollution,” Shi said. whereas the permeability of the aquitard dou- effect of the 2011 Tohoku “If an earthquake causes changes in permea- bled. bility in the aquitard, groundwater may move “As far as I know, this is the first time that earthquake in Japan on upward or downward, thus increasing the risk changes in both an aquifer and an accompany- of groundwater contamination.” ing aquitard have been quantified after an groundwater systems in earthquake,” said Michael Manga, a planetary China. scientist at the University of California, By Mary Caperton Morton (@theblondecoyote), Berkeley who was not involved in the new Science Writer

Earth & Space Science News Eos.org // 11 NEWS

First Persian Gulf Meteotsunami Spotted

onds, the meteotsunami waves arrived every ­15–20 minutes, the scientists calculated. The turbulent were remarkably localized, how- ever, and affected only a roughly 40-kilometer­ section of coastline near the city of Dayyer. Air pressure records from across the Middle East and satellite observations revealed the meteorological conditions that preceded the meteotsunami. Heidarzadeh and his col- leagues found that a tropical cyclone had passed over the region shortly before the first waves were recorded. Such convective storms are characterized by updrafts and downdrafts, which trigger changes in air pressure that can cause . “Atmospheric condi- tions over the [Persian Gulf] were highly favourable for the generation of meteotsuna- mis,” the researchers concluded. Their study was published in July in Pure and Applied Geo- physics (bit.ly/​ pg​ -​​ extreme­ -​ waves).­ “This certainly looks like a classic meteotsunami event and an extremely large one at that,” said Gregory Dusek, a physical oceanographer at the National Oceanic and Atmospheric Administration’s National Ocean Service in Silver Spring, Md., not involved in the study. “It would be valuable to collect a longer time series of water level observations to assess just how rare this type of event is in Meteotsunamis in the Persian Gulf pose a danger to oil infrastructure and low-­ lying​­ homes. Credit: iStock.com/Nikada​­ the Persian Gulf.” There’s hope for predicting meteotsunamis in the Persian Gulf, Heidarzadeh and his col- arthquakes are a common cause of tsu- “When we heard the news…it was a shock,” laborators suggest. Because weather systems namis, but the weather can also be a cul- said Heidarzadeh. tend to move from west to east, meteorologi- E prit when it comes to creating large Seismic activity in the Persian Gulf isn’t cal stations to the west of the inland sea—in waves. Scientists have now analyzed the first strong enough to generate traditional tsuna- Kuwait, Saudi Arabia, Bahrain, and Qatar, for meteotsunami (a portmanteau of “meteoro- mis, and a meteotsunami had never before instance—can be used to track conditions logical ”) to hit the Persian Gulf. This been reported in the area. The event, which conducive to a meteotsunami. That’s good event, which occurred in 2017, is troubling, occurred at roughly 8:00 a.m. local time, killed news because roughly a third of the world’s oil the research team suggests, because so much five people, sank fishing boats, and sent water transported over water passes through this infrastructure, including ­high-​­end resorts and rushing about a kilometer inland. region, and waves that destroy critical infra- ­oil- and gas-­ related​­ equipment, dots the Heidarzadeh and his collaborators have now structure could spell “a disaster for the shoreline of this part of the Middle East. used data and air pressure records to world’s energy supply,” said Heidarzadeh. Mohammad Heidarzadeh, a coastal engi- analyze the waves and the weather conditions He and his colleagues are now creating neer at Brunel University London, and his col- that created them. Using measurements from computer animations of the 2017 meteotsu- leagues first learned about the 19 March 2017 12 gauges in the Persian Gulf, Heidarzadeh nami. They’re using these simulations to meteotsunami through Iranian media outlets. and his team found that waves as large as study how the waves propagated across the 2 meters from crest Persian Gulf, work that informs how to trough—roughly meteotsunamis travel in shallow, protected ­5–10 times larger bodies of water. “We really have to work on u Read the Full Stories than normal—rolled the full reconstruction,” said Heidarzadeh. ashore in southern and the Latest Breaking News Iran. Unlike regular at Eos.org waves, which arrive By Katherine Kornei (@katherinekornei), every 10 or so sec- ­Freelance Science Journalist

12 // Eos October 2019 OPINION

Uncontrolled Chemical Releases: A Silent, Growing Threat

ishing operations in the Gulf of Mexico face a variety of challenges that originate F close to home: hurricanes, leakage from offshore oil rigs, and fishing practices that deplete populations, to name a few. However, they also deal with problems that arise thou- sands of kilometers away. Record flooding in the U.S. Midwest during ­2018–2019​­ has washed everything from Chicago sewage to pesticides and fertilizers from Iowa cornfields down the Mississippi River, fueling algae blooms and the resulting dead zones, includ- ing the one in the Gulf of Mexico. This is just one example of how the uncon- trolled release of household, industrial, and agricultural chemicals into the environment during natural disasters has become a signifi- cant, compounding impact of climate change. Large fluxes of petroleum and ­plastic-​­rich industrial waste, ­nitrogen-laden​­ feedlot and human waste, and pesticide runoff, carried Texas National Guardsmen rescue a Houston resident after Hurricane Harvey in August 2017. Credit: Lt. Zachary West/ into the environment through the air, water, Army National Guard and soil, have the potential to meaningfully damage both ecological and human health [Pierre-­ ​­Louis et al., 2018; Miner et al., 2018b]. of the United States, the , and els of lead and arsenic in hurricane floodwa- These chemicals can be difficult to contain Sudan mobilized fecal matter, chemical run- ters have been repeatedly documented to be when a natural disaster damages storage off, and highway refuse, washing compounds above acceptable limits. These elevated levels structures. However, the effort to control out to sea and mobilizing toxins in the water, can affect the well-­ being​­ of returning resi- chemical discharges is necessary: The cumula- soil, and atmosphere [Schwartz, 2018; Tabuchi dents, compromise the health of near-­ ocean​­ tive impact of these chemical releases has the and Kaplan, 2017]. ecosystems, and take an economic toll on potential to raise background levels of toxic In the United States alone, over 860 cities fishing communities [Appel, 2005; Manuel, substances in the environment all over the use combined sewage overflow systems, which 2006]. world. are designed to release untreated sewage into Nonflood events can also release toxic nearby water bodies during storm or flood chemicals into ecosystems through direct A Pervasive and Growing Problem events. These systems can release up to 700 atmospheric transport. Atmospheric transport As the world observed after the radiation million gallons of overflow per storm event of ash from wildfires like those in California release from the Fukushima Daiichi disaster in [Kenward et al., 2016]. Research has shown that can move household cleaning products, toxic Japan, human-­ made​­ compounds introduced a quantity of E. coli released into a watershed chemicals from building materials, soot, and into the environment are possible to trace after a flood event can proliferate in the water petroleum by-­ products​­ substantial distances [Anzai et al., 2012] but are difficult to control or for up to 3 months [Kapoor et al., 2018], con- through the air [Johnston, 2018; Young et al., fully remediate. Data from Munich Reinsur- tributing to contamination of ecosystems and 2004]. ance, a company that tracks worldwide natural deterioration of human water resources. When summer fires destabilize a region’s disasters, show an increase in all forms of nat- In the fall of 2018, hurricanes in the Ameri- topsoil, winter rains can carry both ash and ural disasters over the past 30 years. Meteoro- can Southeast freed contained chemical efflu- chemicals downstream, affecting the chemical logical and hydrological catastrophes specifi- ent and feedlot waste pools into local ecosys- composition and baseline toxicity of the soil cally have seen greater increases as the tems and the nearby ocean [­Pierre-​­Louis et al., and watershed. In the case of recent California climate has warmed, with events growing 2018]. Although reports on the quantity of wildfires, the cascading impacts were as small from fewer than 300 per year in 1981 to more chemical releases from 2018’s hurricanes are as a change in the taste of regional wines than 600 in 2017. This translates to an inter- still coming out, we know that previous hurri- [Noestheden et al., 2017] and as large as chemi- national increase in hurricanes, strong mon- canes in the American Southeast have released cal transports to glaciers thousands of kilome- soons or flooding events, and droughts. up to 10 million gallons of oil from ­in-ground​­ ters away [Miner et al., 2018a]. In 2018, we saw noteworthy, ­large-scale,​­ storage systems. The U.S. Environmental Pro- unrestricted chemical releases after a number tection Agency (EPA) also counted 65,000 A Cascading Series of Events of different natural disasters. Unprecedented empty hazardous waste containers found after These documented cases illustrate that the summer flooding in Asia, India, the East Coast Hurricane Katrina [Esworthy et al., 2006]. Lev- cumulative impact of uncontrolled environ-

Earth & Space Science News Eos.org // 13 OPINION

mental chemical releases during natural agencies and scale—after Hurricane Irma, Esworthy, R., et al. (2006), Cleanup after Hurricane Katrina: Environ- mental considerations, 30 pp., Congress. Res. Serv., Washington, disasters can create slow and steady increases nearly 43,000 volunteers came forward to help D.C., https://digital.​ library­ .​ unt­ .​ edu/ark:/­ 67531/metacrs9025.​­ in background environmental contaminations those affected in Florida. Johnston, A. (2018), After the fires, rain—and the threat of toxic runoff, to well above current levels. A rise in back- In addition to on-­ the-​­ ground​­ resources, KALW San Francisco, https://www.​ kalw­ .​ org/post/­ after​­ -​ fires­ -​ rain­ -​ and­ ​ -threat­ -​ toxic­ -​ runoff.­ ground toxicity may carry significant ­long-​ cohesive digital tools could help us understand Kapoor, V., et al. (2018), Real-­ time​­ quantitative PCR measurements of ­term health risks, including cancer, impaired the spread of toxins after a release while fecal indicator bacteria and human-­ associated​­ source tracking mark- ers in a Texas river following Hurricane Harvey, Environ. Sci. Technol. reproduction, and immune system damage building a ­data-driven​­ case for incorporating Lett., 5(6), 322–­ 328,​­ https://doi​ .​ org/­ 10​ .​ 1021/­ acs​ .​ estlett­ .​ 8b00237.­ [Birnbaum, 2013; Kortenkamp and Faust, 2018]. the protection of vulnerable facilities into Kenward, A., et al. (2016), Overflow: Climate change, heavy rain, and As hazardous chemicals move through soil, national response plans. Integrating digitally sewage, Clim. Central, Princeton, N.J., http://assets.​­climatecentral​ .org/­ pdfs/​­ Overflow​­ _​ sewagereport­ _​ update­ .​ pdf.­ water, and air and into biota, the potential for enabled big data with applied Kortenkamp, A., and M. Faust (2018), Regulate to reduce chemical toxic biomagnification and bioaccumulation and field monitoring can allow both the public mixture risk, Science, 361(6399), 224–­ 226,​­ https://doi​ .​ org/­ 10​ .​ 1126/­ ​ increases. Bioaccumulation, the absorption of and private sectors to plan for and reduce the science­ .​ aat9219.­ Manuel, J. (2006), In Katrina’s wake, Environ. Health Perspect., 114, chemicals into fat tissue, increases the odds ­long-term​­ impacts of uncontrolled chemical A32–­ A39,​­ https://doi​ .​ org/­ 10​ .​ 1289/­ ehp​ .​ 114­ -​ a32.­ that chemicals released during a past event releases. Miner, K. R., et al. (2018a), A screening-­ level​­ approach to quantifying will move through the human and natural Some of the greatest challenges of this cen- risk from glacial release of organochlorine pollutants in the Alaskan Arctic, J. Exposure Sci. Environ. Epidemiol., 29, 293–­ 301,​­ https://doi​ ​ ecosystems for generations, being transmitted tury could emerge from the secondary and ter- .org/­ 10​ .​ 1038/­ s41370­ -​ 018­ -​ 0100­ -​ 7.­ through breast milk or the consumption of fish tiary impacts of climate change, putting Miner, K., N. Wayant, and H. Ward (2018b), Preventing chemical release in hurricanes, Science, 362(6411), 166, https://doi​ .​ org/­ 10​ .​ 1126/­ and game, for example [Bergonzi et al., 2011]. strains on global resources. Meeting these science.​ aav3822.­ The large quantity and range of chemicals challenges requires governments and risk Noestheden, M., E. G. Dennis, and W. F. Zandberg (2017), Quantitating released in uncontrolled quantities can leave a managers to streamline the process between volatile phenols in Cabernet Franc berries and wine after on-­ vine​­ exposure to smoke from a simulated forest fire, J. Agric. Food legacy of contamination, leading to ­long-term​­ identifying emergent climate risks and ade- Chem., 66(3), 695–­ 703,​­ https://doi​ .​ org/­ 10​ .​ 1021/­ acs​ .​ jafc­ .​ 7b04946.­ health impacts for both humans and animals. quately responding. This, in turn, relies on ­Pierre-Louis,​­ K., N. Popovich, and H. Tabuchi (2018), Florence’s flood- prioritization of accessible, digitally enabled breach coal ash pond and imperil other toxic sites, New York Times, 24 Sept., https://www​ .​ nytimes­ .​ com/­ interactive/​­ 2018/​­ 09/13/​­ ​ Tracking the Toxins planning tools and systems-­ based​­ science. climate/­ hurricane​­ -​ florence­ -​ environmental­ -​ hazards­ .​ html.­ Although the EPA and the European Environ- Even as the world negotiates how to move for- Schwartz, J. (2018), More floods and more droughts: Climate change delivers both, New York Times, 12 Dec., https://www.​ nytimes­ .​ com/­ ​ ment Agency, among others, are making ward with the Paris Agreement, these silent 2018/­ 12/​­ 12/​­ climate/​­ climate​­ -​ change­ -​ floods­ -​ droughts­ .​ html.­ efforts to monitor and record chemical impacts of climate change will continue to Tabuchi, H., and S. Kaplan (2017), A sea of health and environmental releases, further research and real-­ time​­ geo- multiply and compound. hazards in Houston’s floodwaters, New York Times, 31 Aug., https://​ www­ .​ nytimes­ .​ com/­ 2017/​­ 08/​­ 31/us/​­ houston­ -​ contaminated­ -​ floodwaters­ ​ graphically enabled data products are needed. .html.­ Models that incorporate up-­ to-​­ date​­ data with References Young, S., L. Balluz, and J. Malilay (2004), Natural and technologic haz- Anzai, K., et al. (2012), Fukushima Daiichi Nuclear Power Plant ardous material releases during and after natural disasters: A review, geospatial mapping would enable efficient accident: Facts, environmental contamination, possible biological Sci. Total Environ., 322(1–­ 3),​­ 3–­ 20,​­ https://doi​ .​ org/­ 10​ .​ 1016/­ S0048-­ ​ response from agencies and could be incorpo- effects, and countermeasures, J. Clin. Biochem. Nutr., 50(1), 2–­ 8,​­ 9697(03)­ 00446-­ 7.​­ https://doi​ .​ org/­ 10​ .​ 3164/­ jcbn​­ .​ D-­ 11-­ 00021.­ rated into existing monitoring programs. Appel, A. (2005), After Katrina: Tracking the toxic flood, Nature, Combining geospatial data with field 437(7058), 462, https://doi​ .​ org/­ 10​ .​ 1038/­ 437462a.​ Author Information sources or citizen science programs would Bergonzi, R., et al. (2011), Persistent organochlorine compounds in K. R. Miner (kimberley.​ miner@maine­ .​ edu),­ fetal and maternal tissues: Evaluation of their potential influence allow for the development of a digital platform on several indicators of fetal growth and health, Sci. Total Environ., ­University of Maine, Orono for tracking toxic releases, much like easily 409(15), 2,888–­ 2,893,​­ https://doi​ .​ org/­ 10​ .​ 1016/­ j.​ scitotenv­ .​ 2011­ .​ 04­ .​ 031.­ Birnbaum, L. S. (2013), When environmental chemicals act like uncon- accessible weather tracking apps. There is a trolled medicine, Trends Endocrinol. Metab., 24(7), 321–­ 323,​­ https://​ uRead the full story at bit.​ ly/­ Eos​ -​ chemical­ ​ clear precedent for working together across doi.​ org/­ 10​ .​ 1016/j­ .​ tem­ .​ 2012­ .​ 12­ .​ 005.­ -releases­

14 // Eos October 2019 OPINION

mate change. Psychologists Weber and Stern An Evolutionary Leap [2011] attribute this disconnect to two funda- mental factors. First, climate change is intrin- in How We Teach Geosciences sically difficult to understand because of its multiple drivers, consequences, and feed- backs, as well as its operation across different spatial and temporal scales. Second, scientists he content and skills that we teach our and nonscientists develop their understand- geoscience students benefit from devel- ings of the natural world in different ways. T opments in the knowledge and practices Scientists base conclusions and recommenda- of the many research fields within the geosci- tions on data and logic, but for nonscientists, ences. In much the same way, what and how feelings and values often override systematic we teach should be informed by research on observations and measurements of climate geoscience teaching and learning itself—this phenomena. has always been true. However, geoscience It is our job as geoscience educators to break education research is now entering a new down that complexity and help students expe- stage and is poised to take an evolutionary rience how science works. Social science leap [Arthurs, 2019]. If we make this leap suc- research tells us that success likely requires cessfully, teaching practice and student learn- learners to overcome serious obstacles ing will reap the benefits. [Paasche and Åkesson, 2019], such as the tenta- The idea that geoscience education research cles of fake news, groupthink, and failure to (GER) should inform the ways in which geo- think critically [Pennycook and Rand, 2019]. sciences are taught is not new. Eos has been a Currently, there is no consensus in the

venue to share several GER advances, such as © Matsys social science community on how to overcome in how geoscientists think and learn [Kastens these obstacles. However, GER efforts to et al., 2009], methods for teaching geoscience advance climate literacy are under way [e.g., to large classes [Butler et al., 2011], and helping Addressing Stubborn Problems McNeal et al., 2014; Buhr Sullivan and St. John, students develop spatial reasoning skills The questions guiding future research on 2014]. In particular, work by et al. [2017, [Davatzes et al., 2018]. undergraduate geoscience education span a 2018] shows promising results for teaching One next step in this process, the AGU web of topics. These include research on how students how to critically analyze claims about Council’s formation last year of an Education students learn geoscience content, their climate change and inoculate them against section, reflects the value that AGU members development of workforce-­ necessary​­ skills, climate misinformation. place on teaching and learning about Earth. and our ability as instructors to design and These efforts are only the start to closing Education is at the core of nurturing the next implement curricular pathways for the success the gap between the public and scientific generation of diverse Earth scientists, as well of all students [St. John, 2018]. Within these understanding of the high-­ ​­stakes science of as growing public understanding of how Earth areas are stubborn problems that will require climate change. GER is uniquely qualified to science is relevant to everyday and how it action at multiple scales [St. John and McNeal, address this challenge by integrating knowl- helps address pressing problems facing 2017], from case studies to large, ­multi-​ edge about how the Earth system (i.e., the cli- humanity. ­institutional studies, conducted by diverse mate system) works with knowledge about teams of researchers. the theories and methods of social science Grand Challenges for Geoscience Here we give three examples of stubborn research. Education Research problems in the modern landscape of under- Recently, more than 200 geoscience educators graduate geoscience teaching and learning. 2. Complex Problem Solving and researchers engaged in an important Each example highlights needs and opportu- Isn’t What It Used to Be community-­ building​­ and research-­ ​ nities to tackle challenging teaching and When many of us were undergraduates, a ­strengthening process, which spanned a year learning questions of our time by rethinking “problem” was often a ­textbook-​­style exercise and a half. Through a series of National Sci- our assumptions, drawing from new empirical with a single correct answer. This answer ence Foundation–­ funded​­ activities, they data, and applying social science theories and might have been printed in the back of the defined a set of priority research questions, or methods to topics that matter to geoscience textbook, and we could solve the problem “grand challenges,” on 10 themes relevant to educators. using a technique that had been explicitly undergraduate geoscience education. taught in class. Grand challenge exercises have been essen- 1. Overcoming Obstacles In today’s undergraduate geoscience tial steps in other geoscience communities, to Learning High-­ Stakes​­ Science courses, students are increasingly being asked including tectonics research [Huntington et al., Climate change is one of the most widespread to grapple with complex, ­ill-structured​­ prob- 2018] and scientific ocean drilling. When done geoscience challenges facing society today. lems at the intersection between Earth and well, they enable a community to identify This is an example of “­high-​­stakes science,” human systems. Such problems have no single research needs and opportunities going for- which requires a broad response by a scientifi- correct answer and no predetermined pathway ward. This is what the GER community has cally informed populace to avoid potentially toward solutions. Proposed solutions may accomplished. The result is A Community costly and disastrous outcomes. involve values or ethics as well as science and Framework for Geoscience Education Research Compounding the problem and stalling technology. Such work has been called con- [St. John, 2018], a prioritized research agenda possible solutions is the disconnect between vergent science because solutions for prob- and a catalyst for action. the public and scientific understandings of cli- lems must be converged on from different

Earth & Space Science News Eos.org // 15 OPINION

directions. This convergence is difficult to ties of resources that are available for problem sented minority participation is perhaps the teach and learn. solving. Students must learn to navigate this most stubborn problem in geoscience educa- However, we must teach convergent sci- rapidly changing space, identifying and har- tion. Social science theories newly applied to ence, because geoscientists have scientific nessing resources (e.g., tools, data, models, the geosciences [e.g., Callahan et al., 2015, expertise and valuable perspectives needed to experts, collaborators [­Ebert-​­Uphoff and Deng, 2017; Wolfe and Riggs, 2017] are likely going to address a range of economic, environmental, 2017]) that can be brought to bear on the con- be key to developing recruitment and reten- health, and safety challenges [Aster et al., vergent problems. tion strategies for implementation at the indi- 2016]. Research is needed on how societal Employers articulate the importance of vidual and programmatic levels. problems, such as confronting climate vari- using data to solve problems, of learning to ability, ensuring sufficient supplies of clean work on problems with no clear answers, and What Can I Do? water, and building resiliency to natural haz- of managing the uncertainty associated with Geoscience education research on these and ards, can serve as effective contexts for teach- addressing these types of problems. However, other grand challenges identified in the ing and learning in the geosciences. the most effective strategies for learning how framework will strengthen the geosciences as Some help comes from a recent review to manage and extract solutions from large a whole by feeding back into what and how we paper by Holder et al. [2017], which provides a data sets are not clear; therefore, this too is teach. This goal has the underlying assump- conceptual model to guide students in solving among the priorities for geoscience education tions that research results are effectively ­ill-structured​­ problems. This model, which researchers. shared with educators and are used to reform was calibrated against 11 empirical, ­classroom-​ teaching practice. These actions cannot be left ­based research studies, identifies elements of 3. Learning Success to chance—they will require expanding and successful guidance. These elements include and Essential Engagement sustaining dialogue between educators and real-­ world​­ relevance, collaboration among Another set of obstacles to learning is often researchers and increasing support for GER problem solvers, requiring students to analyze overlooked. Imagine a situation in which a across programs and departments. and interpret data, and the possibility to student who did poorly on the last exam AGU members must be part of this effort. At explore more than one pathway to a solution. comes to your office and asks, “How can I bet- the individual level, talk with your colleagues The geoscience education research community ter study for the next one?” You ask, “What who do GER about questions on teaching and has only begun to explore the forms of coach- did you do to prepare for the last exam?” The learning that matter to you. Invite geoscience ing and scaffolding that can help individuals student’s response is typical of many intro- education researchers to your department as who struggle with these types of ­problem-​ ductory college students: “I reviewed the Pow- seminar speakers. At the society level, the based­ curricula. erPoint slides and looked at my textbook.” dialogue can be scaled up by hosting forums Understanding how we can help students Research from the social sciences has where educators can pose questions and talk find and solve Earth­ science–​­related problems shown that students’ ability to reflect on what directly to GER experts and where GER experts that they care about in an ­information-rich​­ they know, what they don’t know, and what can ask questions of educators. society is a high priority for GER. One way we they need to do to improve is vital to the One online model for this is the Research + can make progress is by studying the ­problem-​ learning process, as are their emotions, atti- Practice Collaboratory, an organization that ­finding process itself. Defining authentic tudes, and beliefs. Research addressing these experiments with ways to support mutual cul- problems is not easy, but it is the first critical factors in a geoscience context may be the key tural exchange between researchers and prac- step to solving them. to strengthening the foundation of our under- titioners. Another model, which can be Investigating this process will involve stud- graduate courses. embedded in conferences, is the Geoscience ies on how skilled geoscience problem solvers Results of GER are promising: We have a Education Research and Practice Forum. do their work, how learning occurs during preliminary understanding of what drives In addition, AGU publications can invite problem solving, and what pedagogical some introductory geoscience students to researchers to submit short summaries of new approaches nudge students toward tackling learn new content [van der Hoeven Kraft, 2011] findings and their practical implications for problems as experts do. In addition, people and to study for exams [Lukes and McConnell, teaching topics that align to that journal’s from different backgrounds may perceive and 2014]. However, we need to learn how these focus. Geoscience teaching excellence is a prioritize different problems; therefore, inclu- factors affect students’ abilities to advance shared goal of geoscience educators and geo- sion is especially important in GER around from geoscience novices to geoscientifically science education researchers, and now is the problem solving and in ­problem-based​­ literate citizens or to practicing geoscience perfect time to engage in a disciplinary move- learning. experts. ment forward. We are beginning to explore forms of coach- In addition, the pathways and identities of ing and scaffolding that can help individuals students may affect their emotions, motiva- Acknowledgments struggling with these types of ­problem-based​­ tions, and engagement in our courses. These A Community Framework for Geoscience Edu- curricula (e.g., synthesis work by Holder et al. in turn affect the likelihood of their being cation Research was supported by National [2017]). This research direction is critical attracted to and thriving in the geosciences. Science Foundation grant ­DUE-1708228.​­ With because we anticipate that people who learn Given how geoscience touches the lives of all 48 authors, the framework was truly a collabo- to identify and solve convergent science prob- people, it should also be a field that is repre- rative effort. We invite readers to explore the lems as students will carry that skill set and sentative of all people, but that is not yet the framework in more depth online (­bit​.ly/GER​­ ​ habit of mind into their personal, civic, and case. -framework)­ via the National Association of professional lives. Because geoscience is the least diverse field Geoscience Teachers. Alternatively, the com- The changing landscape of information in science, technology, engineering, and math plete framework, as well as individual chap- technology (e.g., big data, emerging technolo- [Sidder, 2017], with little improvement in ters, can be downloaded from the James Madi- gies, access to a wide variety of tools, rich diversity over the past 4 decades [Bernard and son University Library Scholarly Commons (bit​ multimedia) also affects the kinds and quanti- Cooperdock, 2018], expanding underrepre- .ly/JMU​ -​ library).­

16 // Eos October 2019 OPINION

References Holder, L., H. H. Scherer, and B. E. Herbert (2017), Student learning of Weber, E. U., and P. C. Stern (2011), Public understanding of climate complex Earth systems: A model to guide development of student change in the United States, Am. Psychol., 66, 315–­ 328,​­ https://doi​ ​ Arthurs, L. (2019), Undergraduate geoscience education research: Evo- expertise in problem solving, J. Geosci. Educ., 65(4), 490–­ 505,​­ .org/­ 10​ .​ 1037/­ a0023253.​­ lution of an emerging field ofdiscipline- ­ based​­ education research, https://doi​ .​ org/­ 10​ .​ 5408/­ 17​­ -​ 261.1.­ J. Res. Sci. Teach., 56, 118–­ 140,​­ https://doi​ .​ org/­ 10​ .​ 1002/tea­ .​ 21471.­ Wolfe, B., and E. M. Riggs (2017), Macrosystem analysis of programs Huntington, K. W., et al. (2018), Challenges and opportunities for and strategies to increase underrepresented populations in the Aster, R. C., et al. (2016), Geoscience for America’s critical needs: An research in tectonics: Understanding deformation and the processes geosciences, J. Geosci. Educ., 65(4), 577–­ 593,​­ https://doi​ .​ org/­ 10​ ​ invitation to a national policy dialogue, Am. Geosci. Inst., Alexandria, that link Earth systems, from geologic time to human time. A commu- .5408/­ 17­ -​ 256.1.­ Va., https://www.​ americangeosciences­ .​ org/­ policy/​­ critical​­ -​ needs.­ nity vision document submitted to the U.S. National Science Founda- Bernard, R. E., and E. H. G. Cooperdock (2018), No progress on diver- tion. 84 pp., Univ. of Wash., Seattle, https://doi​ .​­org/10​ ​.­6069/H52R3PQ5. sity in 40 years, Nat. Geosci., 11, 292–­ 295,​­ https://doi​ .​ org/­ 10​ .​ 1038/­ ​ Kastens, K., et al. (2009), How geoscientists think and learn, Eos, Author Information s41561­ -​ 018­ -​ 0116­ -​ 6.­ 90(31), 265–­ 266,​­ https://doi​ .​ org/­ 10​ .​ 1029/­ eost2009EO31.​­ Kristen St. John (mstjohnke@jmu​.­edu), James Buhr Sullivan, S., and K. St. John (2014), Continuation of the theme: Lukes, L. A., and D. A. McConnell (2014), What motivates introductory Madison University, Harrisonburg, Va.; Kelsey Outcomes of climate literacy efforts (part 2), J. Geosci. Educ., 62(4), geology students to study for an exam?, J. Geosci. Educ., 62(4), 535–­ 537,​­ https://doi​ .​ org/­ 10​ .​ 5408/­ 1089​­ -​ 9995­ -​ 62­ .​ 4­ .​ 535­ .​ 1.­ 725–­ 735,​­ https://doi​ .​ org/­ 10​ .​ 5408/­ 13­ -​ 110.1.­ Bitting, Northeastern University, Boston, Mass.; Butler, E. M., P. R. Bierman, and R. H. Gajda (2011), Investigation-­ McNeal, K. S., K. St. John, and S. Buhr Sullivan (2014), Introduction to Cinzia Cervato, Iowa State University, Ames; stimulated discussion sections make geoscience more relevant in the theme: Outcomes of climate literacy efforts (part 1), J. Geosci. large lecture class, Eos, 84(47), 517–­ 522,​­ https://doi​ .​ org/­ 10​ .​ 1029/­ ​ Educ., 62(3), 291–­ 295,​­ https://doi​ .​ org/­ 10​ .​ 5408/­ 1089​­ -​ 9995­ -​ 62­ .​ 3­ .​ 291.­ Kim A. Kastens, ­Lamont-​­Doherty Earth Obser- 2003EO470002.­ Paasche, Ø., and H. Åkesson (2019), Let’s start teaching scientists vatory, Palisades, N.Y.; R. Heather Macdonald, Callahan, C. N., et al. (2015), Using the lens of social capital to under- how to withstand attacks on fact, Eos, 100, https://doi​ .​ org/­ 10​ .​ 1029/­ ​ College of William & Mary, Williamsburg, Va.; John stand diversity in the Earth system sciences workforce, J. Geosci. 2019EO118499.­ McDaris, Science Education Resource Center, Car- Educ., 63(2), 98–­ 104,​­ https://doi​ .​ org/­ 10​ .​ 5408/­ 15­ -​ 083.1.­ Pennycook, G., and D. Rand (2019), Why do people fall for fake news?, Callahan, C. N., et al. (2017), Theoretical perspectives on increasing New York Times, 20 Jan., https://www​ .​ nytimes­ .​ com/­ 2019/​­ 01/​­ 19/​­ ​ leton College, Northfield, Minn.;Karen S. McNeal, recruitment and retention of underrepresented students in the opinion/­ sunday/​­ fake​­ -​ news­ .​ html.­ Auburn University, Ala.; Heather Petcovic, Western geosciences, J. Geosci. Educ., 65(4), 563–­ 576,​­ https://doi​ .​ org/­ 10​ ​ Sidder, A. (2017), Geosciences make modest gains but still struggle .5408/­ 16​­ -​ 238.1.­ with diversity, Eos, 98, https://doi​ .​ org/­ 10​ .​ 1029/­ 2017EO071093.​­ Michigan University, Kalamazoo; Eric Pyle, James Cook, J., S. Lewandowsky, and U. K. H. Ecker (2017), Neutralizing mis- St. John, K. (Ed.) (2018), A Community Framework for Geoscience Madison University, Harrisonburg, Va.; Eric Riggs, information through inoculation: Exposing misleading argumentation Education Research, 155 pp., Natl. Assoc. of Geosci. Teachers, Texas A&M University, College Station; Katherine techniques reduces their influence, PLoS ONE, 12, e0175799, https://​ Northfield, Minn., https://commons.​ lib­ .​ jmu­ .​ edu/­ ger​­ _​ framework/.­ doi.​ org/­ 10​ .​ 1371/­ journal​­ .​ pone­ .​ 0175799.­ St. John, K., and K. McNeal (2017), The strength of evidence pyramid: Ryker, University of South Carolina, Columbia; Ste- Cook, J., P. Ellerton, and D. Kinkead (2018), Deconstructing climate One approach for characterizing the strength of evidence of geosci- ven Semken, Arizona State University, Tempe; and misinformation to identify reasoning errors, Environ. Res. Lett., 13(2), ence education research (GER) community claims, J. Geosci. Educ., 025018, https://doi​ .​ org/­ 10​ .​ 1088/­ 1748​­ -​ 9326/aaa49f.­ 65(4), 363–­ 372,​­ https://doi​ .​ org/­ 10​ .​ 5408/­ 17­ -​ 264.1.­ Rachel Teasdale, California State University, Chico Davatzes, A., et al. (2018), Learning to form accurate mental models, van der Hoeven Kraft, K. J., et al. (2011), Engaging students to learn Eos, 99, https://doi​ .​ org/­ 10​ .​ 1029/­ 2018EO091643.​­ through the affective domain: A new framework for teaching in the u ­Ebert-Uphoff,​­ I., and Y. Deng (2017), Three steps to successful collabora- geosciences, J. Geosci. Educ., 59(2), 71–­ 84,​­ https://doi​ .​ org/­ 10​ .​ 5408/1­ ​ Read the full story at bit.ly/Eos-​teaching­ ​ tion with data scientists, Eos, 98, https://doi​ .​ org/­ 10​ .​1029/­ 2017EO079977.​­ .3543934a.­ -geosciences­ Read it first on

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Earth & Space Science News Eos.org // 17 The Fate of Borneo’s Plunging Tectonic Plates

Scientists installed a dense seismic network to investigate what happens when subduction stops.

By Simone Pilia, Nicholas Rawlinson, Amy Gilligan, and Felix Tongkul

alking around Kota Kinabalu, the capital of the Malaysian state of Sabah in northern Borneo, you cannot help noticing the imposing bulk of Mount Kinabalu. Rising to an elevation of 4,095 meters (13,435 feet), it is among the highest in South- east Asia; it towers over the surrounding Crocker Range (Figure 1), which reaches higher than 2,000 meters. WMount Kinabalu is made of granite that was emplaced within Earth’s crust 7–8 million years ago [Cottam et al., 2010, 2013]. The mountain is a sheeted ­laccolith-​­like body; that is, it initially formed when a mass of magma intruded between two existing rock strata, causing the overlying layers to rise into a dome shape. After the granite was emplaced, it cooled rapidly; scientists have inter- preted this cooling as a reflection of both the granite’s adjustment to ambient crustal tempera- tures and its relatively rapid toward Earth’s surface. The processes responsible for

The Sun peeks over a ridge near the top of Mount Kinabalu in northern Borneo. Credit: Amy Gilligan

18 // Eos October 2019 Earth & Space Science News Sabah is an ideal location to study the process of subduction termination, clearly visible in satellite imagery which is one of the more poorly and digital elevation maps, may at understood stages of the first suggest an , but closer inspection reveals that the global subduction cycle. interior contains a thick sequence of river delta that were deposited at sea level ­10–15 mil​­ - this rapid cooling and how this granitoid body rose so lion years ago. What caused the uplift of southeastern quickly to such spectacular heights remain enigmatic. Sabah and the preceding 10 million years of subsidence, Mount Kinabalu is not the only puzzling geological land- and how were these unusual basins formed? form in Sabah. Travel across the Crocker Range to the The answers to these questions may be found in the southeast of the state, and you will encounter circular postsubduction setting of northern Borneo. As recently as basins that rise up from the surrounding landscape. The 5 million years ago, subduction stopped along the eastern most spectacular of these is Maliau Basin (Figure 1), which margin of Sabah for reasons we do not fully understand. is around 30 kilometers in diameter and is encircled by an The mantle processes and changes in the regional stress imposing ridge up to 1,500 meters high. The basin’s shape, field associated with such an event likely conspired with

Fig. 1. Map of Sabah showing topography and in the background. Yellow and red squares indicate CMG-­ 6TD​­ and CMG-­ 3ESPD​­ seismic sensors, respectively, deployed by the nBOSS research team. The top right inset shows the location of Malaysia (green), with the blue lines depicting the tectonic plate boundaries. The top left inset is a close-­ up​­ of the rectangle, which shows the Maliau Basin (MB). CR = Crocker Range; MK = Mount Kinabalu.

20 // Eos October 2019 Offset (km)

Time (s)

Fig. 2. Vertical component seismograms recorded by the nBOSS net- work from an M6.6 earthquake that occurred about 8,000 kilometers The team hiked to remote locations, including the dense (~5,000 miles) away from the seismic sensors in the Aleutian jungles in the Maliau Basin, to install the seismometer (Alaska) on 15 August 2018. The colored stripes highlight the time peri- network. Credit: Amy Gilligan ods in which body and surface waves are expected to arrive.

surface processes to help shape the landforms we observe duction process came to an end approximately 20 million today. Clearly, we require detailed images of the crust and years ago with the collision of two continents that resulted underlying mantle to understand why subduction ceased in the formation of the Crocker Range. Subsequently, there and how the landforms of Sabah may be related to deeper was a separate system of northward subduction of the processes in the mantle. Celebes Sea beneath eastern Sabah, which ended ­5–6​­ mil- This is where the North Borneo Seismic Survey lion years ago. (nBOSS) project, which involves Borneo’s first temporary The that is now northern Borneo thus bears seismic network, comes into play. The nBOSS project is the the signature of a southeast directed subduction system, result of a collaboration between the University of Cam- followed by a northwest directed subduction system. Con- bridge, the University of Aberdeen, the Universiti Malaysia sequently, Sabah is an ideal location to study the process of Sabah, and the Malaysian Department. In subduction termination, which is one of the more poorly March 2018, we deployed a network of 46 broadband seis- understood stages of the global subduction cycle. mic stations, spaced about 45 kilometers apart, throughout Sabah (Figure 1). This dense cluster of stations comple- Borneo’s First Dense Seismic Network ments the more widely spaced stations in Malaysia’s The nBOSS network, the first of its kind in Borneo, is sup- regional seismic network. plemented by 24 permanent broadband seismic stations that form part of the Malaysian National Seismic Network. Sabah’s Complex Tectonic History To install the instruments in our network, we used ­four-​ Sabah lies near the northeastern edge of ­present-day​­ Sun- ­wheel-​­drive vehicles to make use of all possible roads and daland, the continental core of Southeast Asia, and is sepa- fast motorboats to reach islands in the South China Sea. We dodged leeches as we trekked into the interior of the Maliau Although several models all have merit, Basin and scaled Mount Kinabalu to install an instrument high on the picture is incomplete without some the mountain. The first batch of understanding of how they couple data was successfully recovered in September 2018, and now the with mantle processes. data analysis has begun. The network will record for nearly 2 years. This time frame rated from the Philippines by the Sulu and Celebes Seas. will allow us to record a sufficient number of distant Like much of Borneo, it formed by of continental earthquakes (Figure 2) for the application of a variety of and oceanic material onto the eastern margin of Sundaland seismic imaging techniques, including teleseismic during the Late to early times (~­70–20​­ tomography and receiver function and wave split- million years ago). ting analy​ses. We will extract further surface wave infor- During the Paleogene (~60–25 million years ago), the mation from continuous ambient noise signals. The ­proto–South​­ China Sea was subducted beneath what is now velocity and anisotropy models from this work will pro- the northwestern of Sabah. This sub- vide a number of critical constraints, including crustal

Earth & Space Science News Eos.org // 21 The new tomographic and geodynamic models will provide valuable insight into how continents evolve.

thickness, mantle flow patterns, locations of lithospheric-​ belt. This model can also explain onshore mountain build- ­scale faults, and discontinuities, that will feed into subse- ing and does not require ongoing subduction or under- quent geodynamic modeling. thrusting. The lack of constraints on mantle structure and dynam- What Happens When Subduction Stops? ics beneath Sabah means that published models tend to Recent tectonic activity in Sabah, such as the rapid uplift focus on the crust, and even then, middle to lower crustal and exhumation of Mount Kinabalu [Cottam et al., 2013], structure and processes are often largely based on specu- may be related to subduction termination. However, the lation. Although the aforementioned models all have extent to which postsubduction processes have dictated merit, the picture is incomplete without some under- the evolution of the surface geology in the past ­5–6​­ mil- standing of how they couple with mantle processes. lion years and whether those processes continue to do so On the basis of the presence of recent (~5 million years now are unknown. old) with ocean character in southeastern Several models have been proposed for the crustal evo- Sabah, Hall [2013] proposed three models to explain the lution of the region. One such model posits that localized underlying cause for deformation of the lithosphere and uplift and detachment faulting have caused gravitational vertical movements of the surface: collapse—mountain ranges collapsing under their own detachment of the descending from the rest of the weight—in the Crocker Range, resulting in the formation • plate (slab break off) of the -­ and-​­ thrust​­ belt offshore northwestern Sabah delamination and sinking of the dense root of the litho- [Hall, 2013]. Confirming that gravitational collapse is hap- • sphere into the mantle below pening requires obtaining constraints on the geographic gravitational instability due to a lithospheric drip (a distribution and rates of uplift and linking these to mantle • sinking plume of cold, dense lithospheric material) structure and processes. Another model says that continental extension has For instance, uplift and extension caused by slab break caused orogen collapse and produced a core complex [e.g., off could induce or enhance orogen collapse. Alternatively, Lister and Davis, 1989] with the associated granite intrusion if regional compression has localized strain, then there is manifested by Mount Kinabalu. This model would explain no requirement for any significant mantle anomaly. both offshore subsidence and onshore uplift. Clearly, to properly understand the link between mantle A third model says that a regional compressive stress and crustal processes, a multidisciplinary and multiscale field has localized strain in a foreland ­fold-and-​­ thrust​­ approach is essential.

Mount Kinabalu towers over Kota Kinabalu, capital of the Malaysian state of Sabah in northern Borneo. Credit: Amy Gilligan

22 // Eos October 2019 Linking Field Data and Models The crust and beneath Sabah have yet to be targeted by geophysical imaging studies. The only evi- dence to date comes in the form of global seismic tomog- raphy, which shows a distinct ­high-velocity​­ anomaly in the upper mantle beneath northern Borneo [Hall and Spakman, 2015]. Although this evidence is potentially consistent with a remnant slab or mantle drip, the lack of resolution (>250 kilometers) precludes any further analysis. Through the nBOSS project, we will use a multidisci- plinary approach to address four specific aims: to under- stand mantle dynamics in a postsubduction setting; to determine the existence, cause, and extent of orogen col- lapse; to develop a model for postsubduction evolution of the -­ mantle​­ system; and to unravel the cause of subduction termination in northern Borneo. The new tomographic and geodynamic models will pro- vide valuable insight into how continents evolve. The models we construct for the Sabah region can be com- pared with other recent postsubduction continental envi- ronments, including Europe’s east ­Carpathian-​­Pannonian region, North America’s Baja California, the ­Betic-​­Rif orogen in the western Mediterranean, and the .

Acknowledgments S.P. acknowledges support from Research Council (NERC) grant NE/R013500/1 and from the European Union’s Horizon 2020 research and innova- tion program under Marie ­Skłodowska-​­Curie grant agree- ment 790203. A.G. is supported by a Royal Astronomical Society Research Fellowship. Ten nBOSS seismometers were provided through NERC Geophysical Equipment Facility load 1038. We thank the Malaysian Meteorology Department, Sabah Foundation, and Sabah Parks for logistical support and assistance in the field. We also appreciate support from Guralp Systems Ltd., including provision of additional instruments for deployment on Mount Kinabalu and in Danum Valley.

References Cottam, M., et al. (2010), Pulsed emplacement of the Mount Kinabalu granite, north- ern Borneo, J. Geol. Soc., 167, 49–­ 60,​­ https://doi​ .​ org/­ 10​ .​ 1144/­ 0016­ -​ 76492009­ -​ 028.­ Cottam, M. A., et al. (2013), Neogene rock uplift and erosion in northern Borneo: Evidence from the Kinabalu granite, Mount Kinabalu, J. Geol. Soc., 170, 805–­ 816,​­ https://doi​ .​ org/­ 10​ .​ 1144/­ jgs2011­ -​ 130.­ Hall, R. (2013), Contraction and extension in northern Borneo driven by subduc- tion rollback, J. Asian Earth Sci., 76, 399–­ 411,​­ https://doi​ .​ org/­ 10​ .​ 1016/j­ .​ jseaes­ ​ .2013.04.010.­ Hall, R., and W. Spakman (2015), Mantle structure and tectonic history of SE Asia, Tec- tonophysics, 658, 14–­ 45,​­ https://doi​ .​ org/­ 10​ .​ 1016/j­ .​ tecto­ .​ 2015­ .​ 07­ .​ 003.­ Lister, G. S., and G. A. Davis (1989), The origin of metamorphic core complexes and detachment faults formed during Tertiary continental extension in the northern Colorado River region, U.S.A., J. Struct. Geol., 11, 65–­ 94,​­ https://doi​ .​ org/­ 10​ .​ 1016/­ 0191­ ​ -8141(89)90036­ -​ 9.­

Author Information Simone Pilia (sp895@cam​­ .​ ac­ .​ uk)­ and Nicholas Rawlinson, Department of Earth Sciences, , U.K.; Amy Gilligan, School of Geosciences, University of Aber- deen, U.K.; and Felix Tongkul, Faculty of Science and Natural Resources, Universiti Malaysia Sabah

uRead the full story at bit.​ ly/­ Eos​ -​ subduction­ -​ Borneo­

Earth & Space Science News Eos.org // 23 Korena Di Roma Howley

One hundred fifty years ago, the explorer and scientist argued that the West needed smart development. Now the fast growing region is playing catch-up.

he American West, while steeped in mythology, is also a In the decades that followed, Powell would argue that careful, region that depends heavily on science for its long-term democratic management of water resources in the West must be a livability—and perhaps no one was quicker to realize this crucial component of its development and that a pattern of settle- than John Wesley Powell. A Civil War veteran and an ment and land cultivation based on the 19th-century status quo indefatigable explorer, Powell landed on the national would prove unsustainable. stage in 1869, after an expedition he led became the first to navi- He couldn’t have had a more unreceptive audience. Elected gate the Colorado River’s path through the Grand Canyon. officials, industry titans, and even fellow scientists wanted a nar-

No photos were taken during John Wesley Powell’s pioneering 1869 expedition of the Colorado River. This photo, taken along the Green River in northern Colorado, dates from Powell’s 1871 expedition, which retraced the 1869 journey. Credit: National Park Service

October 2019 Earth & Space Science News Eos.org // 25 rative that better supported the westward march of “prog- “One thing that he didn’t antici- ress,” narrowly defined. pate [was] the degree to which we Fast- forward 150 years, and Powell’s 19th-century would accumulate western soci- appeals are making modern headlines on the strength of ety in big, urban complexes,” their perception and foresight. Even while western states said Jack Schmidt, the Janet lead the nation in economic and population growth—Ari- Quinney Lawson Chair in Colo- zona, Colorado, Nevada, and Utah were among the top five rado River Studies at Utah State states with the fastest growing gross domestic product University and former chief of between 2016 and 2017—drought conditions that have the U.S. Geological Survey’s persisted for decades have left parched cities under con- (USGS) Grand Canyon Monitor- stant threat of water emergencies. ing and Research Center. On the Colorado River, the country’s two largest reser- Powell, Schmidt said, might voirs—Lake Mead, on the border between Nevada and Ari- not have imagined that these zona, and Lake Powell (so named for John Wesley), on the urban complexes “would have John Wesley Powell at age 35, border between Arizona and Utah—are being drained these tentacles that extended the year he led the fi rst expedition faster than they can replenish. The effects of climate way out into the distant land- down the Colorado River and change are only adding to the pressure on limited water scape [or] the degree to which through the Grand Canyon. supplies. these big urban centers would be Credit: USGS In Powell’s account of his explorations, published in maintained by these really long 1895 as Canyons of the Colorado, he describes the river’s canals…these really complicated waters emptying “as turbid floods into the Gulf of Califor- electricity transmission systems nia.” Today only in very wet years does the river reach the that bring in power from distant coal- fired and nuclear ocean. Meanwhile, communities that rely on the Colorado and hydroelectric dam facilities.” for water, including sprawling metropolitan areas like Although Powell’s vision of small communities was Denver, Phoenix, and , are facing the possibil- focused largely on irrigated agriculture, water manage- ity of having their supply cut off or severely limited in a ment, he thought, would be developed at a more local future that’s moving alarmingly nearer. scale. This would, among other benefits, help to hedge against the uncertainties of climate variation. When, for Unforeseen Potential instance, the 1922 Colorado River Compact apportioned It’s tempting, then, to imagine how the West might have shares of Colorado River water to seven states, it was evolved had Powell’s vision for its development been during a particularly wet period, leading to overestimated implemented, rather than shunned, a century and a half water allocations. ago. “One of the big things that would’ve happened if we’d What if Congress, undeterred by the siren song of Amer- listened to Powell is that we…would have responded ear- ican expansion, had listened to the call of the pragmatic? lier to the information about global climate change,” said Would L.A. be a backwater? John F. Ross, author of The Promise of the Grand Canyon: John Would Tucson even appear on the map? Wesley Powell’s Perilous Journey and His Vision for the Ameri- Would the Colorado still rush freely to the gulf from its can West. “He was a great proponent of America’s poten- headwaters in the ? tial; he just wanted to do it in a way that was sensible to Speculation about what might have been is complicated what was on the ground.” by society’s shifting priorities and values, as well as by technology. Powell, for his part, envisioned much smaller When the West Was Young communities dispersed over the western landscape. In 1869, as the post– Civil War United States was knitting itself back into a union, the sparsely settled expanse of states and territories that stretched between the 100th meridian and the Pacific coast was still a great unknown for many Americans. That year, Ulysses S. Grant was inau- gurated as the eighteenth president of the United States, One of the big things that Wyoming became the first U.S. state or territory to grant women suffrage, and a spike driven at Promontory Sum- would’ve happened if we’d mit in Utah connected the country’s first transcontinental railroad. listened to Powell is that we… To many communities in the East and Midwest, the newly accessible West was brimming with possibility and would have responded earlier scarcely tapped resources. John Wesley Powell, then a professor of geology at what is now Illinois State Univer- to the information about sity, had identified an opportunity as he contemplated the last blank spot on the map of the continental United global climate change. States: the Colorado Plateau. Today this area includes Arches, Zion, the Grand Canyon, and five other national parks, as well as nearly two dozen national monuments, historic sites , and recreation areas. In Utah alone, the

26 // Eos October 2019 states’s five national parks brought in 15.2 million visi- tors in 2017. But in the late 19th century it was an altogether different story. When Powell undertook the 3- month descent of the Colorado River in the name of science, the journey was Powell—who had been injured considered by some to be all but suicidal. Still, the retired Union Army major—who had been wounded while fighting while fi ghting in the Battle of in the Battle of Shiloh—conquered the unpredictable Shiloh—conquered the 1, 600- kilometer route with one arm, a small fleet of wooden rowboats, and a cobbled-together team of nine unpredictable 1,600- kilometer willing but inexperienced adventurers. The expedition departed from Wyoming’s Green River route with one arm, a small City on 24 May 1869, with 10 months’ worth of supplies, an optimistic collection of scientific tools, and, among some fl eet of wooden rowboats, and of the men, hopes of finding a fortune. Four men would eventually abandon the expedition, one at the first oppor- a cobbled- together team of tunity and three others less than 2 days before the remain- ing team successfully emerged from the Grand Canyon. nine willing but inexperienced (Those three men were never seen or heard from again.) Although Powell’s scientific ambitions for the expedi- adventurers. tion were largely scuttled by the demands of survival, the widely heralded trip would help to launch his decades- long career as a geologic surveyor, shrewd political player, and government administrator. His recommendations to Con- gress would be instrumental in the creation of the U.S. by train. But the technology that benefited Powell’s plans Geological Survey, and he would later serve a dozen years in 1869 would also facilitate the idealistic expansion that as its director while also leading the Smithsonian’s Bureau he would ultimately spend the latter part of his career of Ethnology and helping to found the Cosmos Club and warning against. the National Geographic Society. The completion of the transcontinental railroad was But it was Powell’s unswaying advocacy for land and especially timely for a nation in pursuit of Manifest Des- water management in the West that would prove to be one tiny, which disregarded the realities of climate and the of his most remarkable legacies. native peoples who occupied the land in favor of spreading American industrialism and progress from coast to coast. A Watershed Idea Politicians, speculators, and homesteaders were eager to It was the railroad that made it possible for Powell and his exploit the promise of the West’s seemingly endless team to launch the expedition from the banks of the Green resources and would be quick to deny the hard truth that River. The conveniently located station at Green River City lives and livelihoods depended on one all- important ingre- meant that Powell could easily bring his boats and supplies dient: water. In his 1879 Report on the Lands of the Arid Region of the United States, with a More Detailed Account of the Lands of Utah, with Maps, Powell foresaw the consequences of applying Ameri- can optimism—and opportunism—in a part of the country where annual rainfall measured below 50 centimeters. He warned that there wasn’t enough water to support large- scale farming or the rapid settlement of federal lands stimulated by the Homestead Act of 1862. In addition, the costs of establishing effective irrigation systems threatened to keep control out of the hands of small farmers. Certain conditions, Powell said, had to be met to develop the region successfully, includ- ing the identification of irrigable areas and local control of dam and irrigation projects. It was a position Powell would refuse to abandon. While testifying before a congressional committee in 1890, when he was head of the Powell’s expedition down the Colorado was honored by the U.S. Postal Service on the USGS, Powell deployed a unique visual aid: a expedition’s centenary in 1969. Credit: U.S. Bureau of Engraving and Printing, Smithso- map that divided the western states and terri- nian National Postal Museum tories into a series of drainage districts.

Earth & Space Science News Eos.org // 27 On first viewing, it’s a surprising example of 19th- century cartography, made all the more striking with rich colors and irregular, organic- looking boundaries that con- trast sharply with the boxy borders we’re familiar with today. Powell introduced the idea that But the schematic didn’t hold water, so to speak, with a nation determined to grow and expand. The outlook of the arid cultures either stood or nation was invested in myths that encouraged develop- ment and defied science, whereas Powell, Schmidt said, fell…not on the absolute amount lacked the tolerance for pursuing such myths, including the widely held belief that “rain follows the plow.” of water, but on how In 1902, the year Powell died, Congress passed the Rec- lamation Act to “reclaim” the arid region for agriculture equitably—politically and and settlement. “That set the stage for this really large- scale water economically—the system development in the West that almost defied the function- divided that resource. ing of the watershed from an ecological perspective,” said Sandra Postel, founder and director of the Global Water Policy Project and author of Replenish: The Virtuous Cycle of Water and Prosperity.

Powell’s expedition down the Colorado River departed from Green River City, Wyo., on 24 May 1869 and ended at the far side of the Grand Canyon 99 days late r. Credit: As director of the USGS in 1890, Powell presented this map of western watersheds Schwabenblitz/Shutterstock.com; Cartarium/Shutterstock.com; Design: Potomac Com- (drainage districts) to Congress. Credit: USGS munications Group

28 // Eos October 2019 Said Ross, “We’re seeing this kind of bioregionalism now, where decisions are made not by the federal govern- ment but on a more local, or regional, basis—[which is] really the only way to work out these very knotty issues.” Postel said that successful restoration often involves collaboration, such as conservationists working with farm- ers to find solutions to water management issues. “If we get smarter about using and managing water, we can do better with what we’ve got than we’re currently doing,” she said. As the challenges and accomplishments of western set- tlement continue to ebb and flow, Powell’s influence still lingers. Like Postel, Schmidt believes that the key to water man- agement in the West is in working together as a watershed community. “In a sense, that’s an idea of Powell’s that still exists today,” he said. “It’s just that the community that we call the watershed includes the entire Colorado River basin. It includes every one of the seven states, all sitting around the table together.”

Author Information Korena Di Roma Howley (korenahowley@gmail . c om), Freelance Journalist

uRead the full story at bit.ly/Eos- Powell

This boat, the Emma Dean, carried Powell and his characteristic chair down the Colorado in 1872. Credit: National Park Service

Today, “the river is really operated more according to needs for hydropower, flood control, irrigation, and water supply,” Postel said. “You couldn’t have cities like Las www.bartington.com Vegas and Los Angeles and Phoenix and Tucson without this extra water.” INSTRUMENTATION FOR In the Same Boat ENVIRONMENTAL MAGNETISM Although Powell’s insistence on viewing the West’s water problem with scientific objectivity was deeply unpopular at MS2/MS3 the time, today it’s apparent that his approach was Magnetic Susceptibility Equipment forward- thinking. Now science is taking a leading role in -6 helping to reclaim the region for the environment while • Resolution to 2x10 SI facilitating ways for a growing population to live there sus- • Laboratory sensor with dual tainably. frequency facility Powell believed that “science is a process of continually • Core logging and scanning sensors • Field survey equipment improving the details of our understanding of natural pro- cesses, and he would be very proud of the role of science in informing river management and protection,” said Schmidt. US distributor: ASC Scientifi c According to Ross, Powell set the stage for the type of E: sales@ascscientifi c.com conversation we should be having about our natural W: www.ascscientifi c.com resources. “He introduced the idea that arid cultures either stood or fell…not on the absolute amount of water, but on how equitably—politically and economically—the system divided that resource,” he said. And what lessons can be taken from Powell as the West moves forward?

Earth & Space Science News Eos.org // 29

EOS-AD-April-2019.indd 1 30/04/2019 09:55 Understanding Alaska’s Earthquakes

One of the longest deployments of new seafl oor seismograph technology was just completed— and you can get the data now.

By G. A. Abers, A. N. , Peter J. Haeussler, Emily Roland, P. J. Shore, Douglas A. Wiens, Susan Y. Schwartz, Anne F. Sheehan, D. J. Shillington, Spahr Webb, and Lindsay L. Worthington

NORTH AMERICA’S LARGEST EARTHQUAKES and most powerful volcanic eruptions occur along the Alaska Penin- sula subduction zone, a meeting of two tectonic plates that sweeps an arc across the North Pacific margin between Alaska and Russia. However, studies that would help us understand these hazards are few and far between in this remote, sparsely populated region. A major new shoreline- crossing community seismic experiment spans the Alaska Peninsula subduction zone, with the intention of filling gaps in our knowledge of this region. Information that we collect along this margin can provide direct infor- mation about many first- order questions about subduction zone processes that influence earthquakes and . For example, segments that have generated great earthquakes (M > 9) behave very differently than segments that are smoothly creeping, and various arc seg- ments have fundamentally different . If we can understand how

Recovery of a shallow-water ocean bottom seismometer, by R/V Jason, with the volcanoes of the Alaska Peninsula in background. Photo Credit A. Adams

30 // Eos October 2019 Earth & Space Science News Eos.org // 31 Fig. 1. Map of the AACSE deployment and the southwestern Alaska margin, showing newly deployed (circles) and existing (squares) seismometers, rupture areas of great earthquakes (orange, labeled with dates), volcanoes (triangles), and other features. Abbreviations are TA/AEC, Transportable Array/Alaska Earthquake Center; AVO, Alaska Volcano Observatory; OBS, ocean bottom seismometer; and APG, absolute pressure gauge.

geologic structures or material properties contribute to this array covered an ­along-strike​­ segment of the subduction segmentation, then we should be able to better forecast zone spanning some 650 kilometers, including the Alaska the ­long-term​­ rates and effects of major geological events. Peninsula and Kodiak Island, and it extended about 250 Historically, geophysical data collection has been chal- kilometers seaward from the . lenging in Alaska because of difficult logistics; low popula- The array densified and expanded offshore the Earth- tion density; and, like most subduction zones, the chal- Scope Transportable Array, a major community experiment lenge of extending comprehensive studies offshore to that is running concurrently. This is a golden age for include the fore arc and subducting plate. The Alaska instrumental seismology in Alaska with the full deploy- Amphibious Community Seismic Experiment (AACSE) has ment of the Transportable Array, AACSE, and several other deployed an amphibious seismic array, designed by the projects. scientific community, to make major advances on these AACSE stems in part from a 2014 workshop on the future problems. This array is recording earthquakes and other of amphibious seismology and in part from science plans events in the Alaska subduction system as well as globally. for two National Science Foundation research programs, All these data are made available openly as rapidly as pos- Geodynamic Processes at Rifting and Subducting Margins sible, to make it as easy as possible for scientists around (GeoPRISMS) and EarthScope. In different ways, both of the world to become involved. these decadal programs have a strong focus on under- standing subduction systems, and both use North America AN AMPHIBIOUS ARRAY as a natural laboratory for fundamental discovery. The AACSE deployed an array of 75 broadband ocean bottom AACSE project also builds on valuable lessons learned from seismometers (OBSs) and 30 onshore broadband seismom- the Cascadia Initiative, a ­4-year​­ series of linked OBS eters from May 2018 to September 2019 (Figure 1). The deployments farther south, across and around the Juan de

32 // Eos October 2019 Fig. 2. Ocean bottom seismometers used in AACSE. A ­shallow-water​­ instrument (left). Dan Kot prepares a deepwater OBS for deployment (right). Credits: David Heath (left); Anne Sheehan (right)

Fuca and Gorda plates, in which much of the AACSE work with amphibious data sets. Each deployment or instrumentation was developed [Toomey et al., 2014]. recovery cruise included multiple ­early- to middle-­ career​­ A critical part of AACSE is its amphibious nature: tight scientists without prior marine experience. Cruise partici- integration of onshore and offshore observational cam- pants ranged from graduate students to faculty to geosci- paigns. Virtually all subduction systems on Earth span the ence professionals to Alaskan high school science educa- shoreline, from deep submarine trenches to large subaerial tors, all of whom gained invaluable direct experience with volcanoes (i.e., volcanoes that erupt into the air rather data collection. An undergraduate short course was held in than in water). Consequently, subduction systems call for Kodiak during fieldwork. In these ways, AACSE provides a observational approaches that extend onshore and at sea. major new data set and helps build the community that can However, science planning and funding often place artifi- make use of it, maximizing the potential impact of this cial barriers at the shoreline, making truly amphibious community resource. projects rare. The AACSE program has worked hard to leverage resources from NSF’s terrestrial (Division of Earth THE 2018 DEPLOYMENT Sciences) and marine (Division of Ocean Sciences) pro- The heart of the AACSE project was a network of 105 broad- grams, and it has focused on integrated planning at every band seismometers and numerous accelerometers, sea- step. floor pressure gauges, and temperature sensors deployed every ­20–50​­ kilometers along the seafloor and on land. We A COMMUNITY EXPERIMENT deployed 75 ocean bottom seismometers on two cruises on AACSE is a “community” project in several ways. First, all the R/V Sikuliaq, sailing from the home port of Seward, data from the project are made openly accessible to any Alaska, with support from OBS facilities at the ­Lamont-​ interested scientist as soon as they are recovered from the ­Doherty Earth Observatory of and the field and formatted for archiving. All seismograms are Woods Hole Oceanographic Institution (WHOI). Twenty of available at the Incorporated Research Institutions for the OBSs have ­trawl-resistant​­ mounts especially designed Seismology (IRIS) Data Management Center, which han- for shallow water, protected against bottom trawling, and dles a wide range of seismic data and data access plat- designed to dampen wave and current noise (Figure 2). Five forms. Other data are housed in appropriate data centers of these OBSs have accelerometers to record nearby strong for their data types; for instance, shipboard data are at the earthquakes. All OBSs were recovered by the Sikuliaq, with Marine Geoscience Data System. The AACSE web page has support from WHOI’s R/V Jason, and the R/V Marcus G. specifics on the program and data access (bit​.ly/­ ​­aacse). Langseth. Second, the experimental planning, design, and partici- In parallel with the marine expeditions, ground teams pation have been kept as open as possible. A large plan- deployed 30 broadband land stations on Kodiak Island, the ning meeting in 2014 evaluated a wide variety of scientific Alaska Peninsula, and the Shumagin Islands, using a vari- targets, followed by several ­web-based​­ forums, open calls ety of small planes, boats, and wheeled vehicles to reach for principal investigator participation, and public com- critical locations in this remote region. These instru- ment periods once draft deployment designs were crafted. ments, provided by the IRIS Portable Array Seismic Stud- Third, the project engages and trains the next genera- ies of the Continental Lithosphere (PASSCAL) Instrument tion of scientists by teaching them the skills required for Center, feature broadband seismic sensors designed for postholes, and six include accelerometers. The distribu- tion of the onshore stations was designed to complement the marine deployment, the sparse permanent networks “Historically, geophysical in this region, and the EarthScope Transportable Array. All broadband sensors have ­120-​­second response corners, data collection has been and they collect data continuously at a frequency of 100 hertz. challenging in Alaska.” In May 2019, AACSE deployed a dense array of approxi- mately four hundred 5-­ hertz,​­ three-­ component​­ “nodal” seismometers across the road system on Kodiak, which sits

Earth & Space Science News Eos.org // 33 Sunset from the R/V Sikuliaq, July 2018. Broadband ocean bottom seismometers arranged on deck are ready to be deployed in support of the Alaska Amphibious Community Seismic Experiment. Credit: Anne ­Sheehan

atop the rupture zone of the great (M9.2) 1964 Alaska WP24 HHE earthquake. This relatively new technology adopted from WP24 HHN

the petroleum industry allows significant oversampling of WP24 HHZ

the high-­ frequency​­ wavefield to enable high-­ resolution​­ WP25 HHE

studies of the thrust zone structure and associated micro- WP25 HHN

earthquakes. While this dense array was deployed, the WP25 HHZ

active-­ source​­ system aboard the Langseth was deployed for WP30 HHE

17 days of high-­ resolution​­ wide-­ angle​­ imaging across WP30 HHN

much of the AACSE array. WP30 HHZ

The community nature of AACSE has also inspired a WS26 HHE

series of side projects and ­follow-on​­ projects, including WS26 HHN

deployments of seafloor GPS-­ acoustic​­ stations, ­next-​ WS26 HHZ ­generation absolute pressure gauges, seafloor temperature WS28 HHE observations linking to the above, and sub- WS28 HHN 60 s seafloor electromagnetic imaging. WS28 HHZ 04:11:00. 04:12:00. 04:13:00. 04:14:00. 04:15:00. 04:16:00. 04:17:00. 04:18:00. 04:19:00. 04:20:00. 04:21:00. 04:22:00. 04:23:00.

A 15-­ MONTH​­ SNAPSHOT Fig. 3. Example seismograms recorded on 24 June 2018 for three earthquakes ( M3.6, The ­15-month​­ deployment of AACSE stations represents M4.5, and M4.3) across five western peninsula AACSE land stations. Raw data were fil- one of the longest ­large-​­scale ­multi-​­instrument amphib- tered to include only 2- to­ 15-hertz­ energy. These earthquakes occurred on the western ious seismic deployments to date. The instrument centers portion of the Semidi segment. that engineered the OBSs designed them to accommodate a ­two-​­summer deployment duration specifically for this experiment. Even this extended deployment time provides only a generates earthquakes at very high rates and from differ- snapshot of the earthquake cycle, but this snapshot has ent sources: along the plate boundary interface, within the captured much of interest. The Alaska Peninsula region downgoing plate, and within the overriding ­fore-arc​­ crust.

34 // Eos October 2019 The 15-month deployment of AACSE stations will represent one of the longest large-scale multi-instrument amphibious seismic deployments to date.

During the AACSE deployment, the Shumagin region experienced several swarms of earthquakes, including many M > 5 events, and other large events (M­ 4–​­5) have happened north of Kodiak Island and within the central Semidi segment (e.g., Figure 3). At the far eastern extent of the array, an ongoing aftershock sequence of the Janu- ary 2018 M7.9 earthquake within the was also recorded at close range using offshore instruments. Col- lectively, this experiment recorded abundant seismic activity, which should provide new insight into earth- quake source properties and serve as a source for local geophysical imaging.

INTEGRATING OBSERVATIONS ON LAND AND SEA Although broadband array seismology has greatly advanced our understanding of Earth beneath continents since the early 1990s, the capability to deploy large arrays at sea has existed only for the past few years. Yet the most seismogenic places are largely offshore or cross coastlines, and understanding the 60% of Earth beneath can be done only from the seafloor. AACSE is a major advance in addressing these challenges with new and emerging technologies. Information on AACSE, including regular updates on progress and participation opportunities, is available at the project’s GeoPRISMS-­ hosted​­ website (bit.​ ly/­ aacse).​­ AACSE data are archived at the IRIS Data Center under network codes XO for onshore sites and XD for OBSs.

ACKNOWLEDGMENTS (top) Susan Schwartz services a land-based instrument station on Alas- AACSE is supported by National Science Foundation award ka’s Kodiak Island as a part of AACSE. Credit: Daniel Sampson. (bottom) ­OCE-1654568,​­ with instrumentation and data management Graduate student Amanda Price inspects a seismometer in preparation support from IRIS and the Ocean Bottom Seismometer for the AACSE deployment off Kodiak. Credit: Bethany Essary Instrument Center. Anne Bécel led the active-­ ​­source acquisition leg. We thank the many support staff onshore and on the R/V Sikuliaq and R/V Langseth and the apply-­ to-​­ ​ ­sail participants who made this deployment possible. of Washington, Seattle; P. J. Shore and Douglas A. Wiens, Department of Earth and Planetary Sciences, Washington REFERENCES University in St. Louis, Mo.; Susan Y. Schwartz, Department Toomey, D. R., et al. (2014), The Cascadia Initiative: A sea change in seismological studies of Earth and Planetary Sciences, University of California, Santa of subduction zones, Oceanography, 27(2), 138–­ 150,​­ https://doi​ .​ org/­ 10​ .​ 5670/­ oceanog​­ ​ .2014.­ 49.­ Cruz; Anne F. Sheehan, Department of Geological Sciences, University of Colorado Boulder; D. J. Shillington and Spahr AUTHOR INFORMATION Webb, ­Lamont-​­Doherty Earth Observatory, Columbia Univer- G. A. Abers (abers@cornell.­edu), Department of Earth and sity, Palisades, N.Y.; and Lindsay L. Worthington, Department Atmospheric Sciences, , Ithaca, N.Y.; A. N. of Earth and Planetary Sciences, University of New Mexico, Adams, Department of Geology, Colgate University, Hamilton, Albuquerque N.Y.; Peter J. Haeussler, U.S. Geological Survey, Anchorage, Alaska; Emily Roland, School of Oceanography, University uRead the full story at bit.ly/Eos-Alaska​­ -​earthquakes­

Earth & Space Science News Eos.org // 35 AGU NEWS

Earth and Planetary Surface Processes 2019 AGU Section Awardees Section G. K. Gilbert Award in Surface Processes and Named Lecturers Kelin X. Whipple, Arizona State University Luna B. Leopold Young Scientist Award Joel S. Scheingross, University of Nevada, Reno

he 2019 section awardees and named lecturers have been selected, and AGU staff, leaders, Robert P. Sharp Lecture and selection committees wholeheartedly congratulate these awardees! Joel S. Scheingross, University of Nevada, Reno Our colleagues have been selected for these prestigious honors for their sustained and T Earth and Space Science Informatics unique contributions to advancing our understanding of Earth, its atmosphere and , and planets and astral bodies beyond our own. The sciences encompassed by AGU are crucial for the Section Greg Leptoukh Lecture health and well-being of our planet’s inhabitants. These awardees have contributed to both that understanding and the planetary health and well-being through their scientific advancements Barbara Jane Ryan, Group on Earth and outstanding service to the science and to AGU. Observations (Former Director) This year’s cohort of awardees reflects the diversity that is integral to the Earth and space sci- Geodesy Section ences. Among the 25 sections of AGU there are 65 such awards; 21 are for early-career scientists John Wahr Early Career Award (up to 10 years post-Ph.D.) and 6 are for midcareer (10–20 years post-Ph.D.). Twenty-seven Raphaël Grandin, Institut de Physique du awards provide named lectureships that offer unique opportunities to highlight the meritorious Globe de Paris, Université de Paris accomplishments of the awardees. AGU inaugurated the Bowie Lecture in 1989 to commemorate the fiftieth presentation of the Medal, which is named for AGU’s first president Ivan I. Mueller Award for Distinguished Service and is the highest honor given by the organization. In the list below, asterisks denote Bowie lec- and Leadership turers. Named lectures offered by AGU sections recognize distinguished scientists with proven Frank Flechtner, GFZ German Research leadership in their fields of science. We look forward to attending as many of these lectures as Centre for Geosciences possible at Fall Meeting 2019 and encourage everyone to mark their calendars with these events. William Bowie Lecture* Many, many thanks to the nominators, nomination supporters, section leaders, and, particu- Véronique M. A. Dehant, Royal Observatory larly, the selection committees for their important work in selecting these well-deserving col- of Belgium leagues. We thank you all for your continued commitment to the AGU Honors Program. We look forward to recognizing the honorees and their achievements at AGU’s Fall Meeting 2019 in San Geomagnetism, Paleomagnetism, Francisco, Calif. and Electromagnetism Section Suzanne A. McEnroe, Norwegian University By Robin , President and Council Chair, AGU; and Mary Anne Holmes (agu_unionhonors@agu​­ ​ of Science and Technology .org), Chair, Honors and Recognition Committee, AGU Edward Bullard Lecture* Gauthier Hulot, Institut de Physique du Atmospheric and Space Electricity Section Future Horizons in Climate Science: Turco Globe de Paris, Université de Paris Benjamin Franklin Lecture Lectureship Joseph R. Dwyer, University of New Hampshire Alex Hall, University of California, Los Global Environmental Change Section Angeles Bert Bolin Global Environmental Change Award Atmospheric Sciences Section and Lecture Atmospheric Sciences Ascent Award Biogeosciences Section L. Ruby Leung, Pacific Northwest National Francina Dominguez, University of Illinois Thomas Hilker Early Career Award for Laboratory at Urbana-Champaign Excellence in Biogeosciences Global Environmental Change Early Career Award Jennifer G. Murphy, Kimberly A. Novick, Indiana University Gretchen Keppel-Aleks, University of David Noone, Oregon State University Bloomington Michigan Ann Arbor Armin Sorooshian, University of Arizona Abigail L. S. Swann, University of Rainer M. Volkamer, University of Colorado Sulzman Award for Excellence in Education Washington Boulder and Mentoring Rebecca T. Barnes, Colorado College Yangyang Xu, Texas A&M University James R. Holton Award Piers J. Sellers Global Environmental Change Nadir Jeevanjee, Princeton University William S. and Carelyn Y. Reeburgh Lecture Mid-Career Award Colleen Hansel, Woods Hole Oceanographic Yoram J. Kaufman Outstanding Research and Katherine V. Calvin, Pacific Northwest Institution Unselfish Cooperation Award National Laboratory Allen H. Goldstein, University of California, Cryosphere Sciences Section Stephen Schneider Lecture Berkeley Cryosphere Early Career Award Andrew E. Dessler, Texas A&M University Jacob Lecture* Natalya Gomez, McGill University Tyndall History of Global Environmental Change Cecilia M. Bitz, University of Washington John F. Nye Lecture Lecture Jule Gregory Charney Lecture* Helen Amanda Fricker, Scripps Institution William D. , Lawrence Berkeley Neil McPherson Donahue, Carnegie Mellon of Oceanography, University of National Laboratory and University of University California, San Diego California, Berkeley

36 // Eos October 2019 AGU NEWS

Hydrology Section Ocean Sciences Award Study of the Earth’s Deep Interior Hydrologic Sciences Early Career Award Paula S. Bontempi, NASA Section Megan Konar, University of Illinois at Study of the Earth’s Deep Interior Section Award Rachel Carson Lecture Urbana-Champaign for Graduate Research Heidi M. Sosik, Woods Hole Oceanographic Di Long, Tsinghua University Neala Creasy, Yale University Institution Kaveh Madani, Yale University Wenbo Wu, Princeton University and Harald Sverdrup Lecture California Institute of Technology Hydrologic Sciences Award Mary-Louise Timmermans, Yale University William P. Kustas, Agricultural Research Tectonophysics Section Service, U.S. Department of Agriculture Paleoceanography and Paleoclimatology Jason Morgan Early Career Award Walter Langbein Lecture* Section Jacqueline Austermann, Columbia Efi Foufoula-Georgiou, University of Willi Dansgaard Award University Valerie Trouet, University of Arizona California, Irvine Francis Birch Lecture* Paul A. Witherspoon Lecture Harry Elderfield Outstanding Student Paper Award Claudio Faccenna, Roma TRE University Patrick M. Reed, Cornell University Jianghui Du, Oregon State University Volcanology, Geochemistry, Horton Research Grant Nanne Weber Early Career Award and Petrology Section Bronwen L. Konecky, Washington David Litwin, Johns Hopkins University Hisashi Kuno Award University in St. Louis Magali Furlan Nehemy, University of Marion Garçon, Centre National de la Saskatchewan Planetary Sciences Section Recherche Scientifique–Laboratoire Lorenzo Rosa, University of California, et Volcans Clermont-Ferrand Ronald Greeley Early Career Award in Planetary Berkeley Daniel A. Stolper, University of California, Sciences Berkeley Mineral and Rock Physics Section Xi Zhang, University of California, Santa Cruz Norman L. Bowen Award and Lecture Mineral and Rock Physics Early Career Award Fred and Lecture Graham Pearson, University of Alberta Sergey S. Lobanov, GFZ German Research Faith Vilas, Planetary Science Institute Centre for Geosciences Mary R. Reid, Northern Arizona Eugene Shoemaker Lecture* University Mineral and Rock Physics Graduate Research S. Alan Stern, Southwest Research Institute Award Reginald Lecture* Kathryn M. Kumamoto, University of Oxford Seismology Section Marie Edmonds, University of Cambridge Christopher Thom, University of Keiiti Aki Early Career Award Joint Award: Geodesy, Seismology, Pennsylvania Zachary E. Ross, California Institute of and Tectonophysics Sections Technology John C. Jamieson Student Paper Award Paul G. Silver Award for Outstanding Scientific Suyu Fu, University of Texas at Austin Beno Gutenberg Lecture* Service Francesca Miozzi, Institut de Minéralogie, Emily E. Brodsky, University of California, Judith Savaso Chester, Texas A&M de Physique des Matériaux et de Santa Cruz University Cosmochimie Space Physics and Aeronomy Section Joint Prize: Nonlinear Geophysics Natural Hazards Section Basu United States Early Career Award for and Space Physics and Aeronomy Natural Hazards Section Award for Graduate Research Excellence in Sun-Earth Systems Sections Research Science Space Weather and Nonlinear Waves and Sanne Muis, Vrije Universiteit Amsterdam Evan G. Thomas, Dartmouth College Processes Prize Michael Hesse, University of Gilbert F. White Distinguished Award and Fred L. Scarf Award Lecture Terry Zixu Liu, University of California, Joint Lecture: Biogeosciences and Jeroen Aerts, Vrije Universiteit Amsterdam Los Angeles Planetary Sciences Sections Carl Sagan Lecture Near-Surface Geophysics Section Space Physics and Aeronomy Richard Education and Public Outreach Award Penelope J. Boston, NASA Ames Research GSSI Student Grant Nat Gopalswamy, NASA Goddard Space Center Zachariah Seaman, Southern Illinois Flight Center University Joint Lecture: Paleoceanography Sunanda and Santimay Basu (International) and Paleoclimatology and Ocean Sciences Nonlinear Geophysics Section Early Career Award in Sun-Earth Systems Sections Donald L. Turcotte Award Science Cesare Emiliani Lecture Vera Melinda Galfi, University of Hamburg Ajeet Kumar Maurya, Doon University Hai Cheng, Xi’an Jiaotong University Ed Lorenz Lecture Lecture* Joint Student Grant: Atmospheric Ian Main, University of Edinburgh Margaret “Peggy” Ann Shea, Air Force Sciences and Space Physics and Research Laboratory (Ret.) Ocean Sciences Section Aeronomy Sections Ocean Sciences Early Career Award Marcel Nicolet Lecture* Edmond M. Dewan Young Scientist Scholarship Nicole S. Lovenduski, University of Colorado Cora E. Randall, University of Colorado Nikita Aseev, GFZ German Research Centre Boulder Boulder for Geosciences

Earth & Space Science News Eos.org // 37 AGU NEWS

Ruth A. Harris , Earthquake Science Center, 2019 Class of AGU Fellows U.S. Geological Survey Robert M. Hazen, Carnegie Institution for Announced Science Kosuke Heki, Hokkaido University Karen Heywood, University of East Anglia Russell Howard, United States Naval Research ach year since 1962, AGU has elected as Fellows members whose visionary leadership and Laboratory scientific excellence have fundamentally advanced research in their respective fields. This Alan G. Jones, Complete MT Solutions Inc. E year, 62 members will join the 2019 class of Fellows. and Dublin Institute for Advanced Studies AGU Fellows are recognized for their scientific eminence in the Earth and space sciences. Kurt O. Konhauser, University of Alberta Their breadth of interests and the scope of their contributions are remarkable and often ground- Sonia Kreidenweis, Colorado State University breaking. Only 0.1% of AGU membership receives this recognition in any given year. Kitack Lee, Pohang University of Science On behalf of AGU’s Honors and Recognition Committee, our Union Fellows Committee, our and Technology section Fellows committees, AGU leaders, and staff, we are immensely proud to present the 2019 Zheng-Xiang Li, Curtin University class of AGU Fellows. Jean Lynch-Stieglitz, Georgia Institute We appreciate the efforts of everyone who provided support and commitment to AGU’s Hon- of Technology ors Program. Our dedicated AGU volunteers gave valuable time and energy as members of selec- Kuo-Fong Ma, National Central University tion committees to elect this year’s Fellows. We also thank all the nominators and supporters and Academia Sinica who made this possible through their dedicated efforts to nominate and recognize their col- Reed Maxwell, Colorado School of Mines leagues. John W. Meriwether, Clemson University (Emeritus) and New Jersey Institute of Honor and Celebrate Eminence at Fall Meeting Technology At this year’s Honors Tribute, to be held Wed­nesday, 11 December, at Fall Meeting 2019 in San Son V. Nghiem, Jet Propulsion Laboratory, Francisco, Calif., we will celebrate and honor the exceptional achievements, visionary leader- California Institute of Technology ship, talents, and dedication of 62 new AGU Fellows. Yaoling Niu, Durham University Please join us in congratulating our 2019 class of AGU Fellows, listed below in alphabetical Thomas H. Painter, Joint Institute for Regional order. Earth System Science and Technology, University of California, Los Angeles Beth Parker, University of Guelph By Robin Bell, President, AGU; and Mary Anne Holmes ([email protected]), Chair, Honors and Ann Pearson, Harvard University Recognition Committee, AGU Graham Pearson, University of Alberta Lorenzo M. Polvani, Columbia University in the City of New York Zuheir Altamimi, Institut National de Peter Reiners, University of Arizona l’Information Géographique et Forestière Yair Rosenthal, Rutgers University– and Institut de Physique du Globe de Paris New Brunswick Ronald Amundson, University of California, Osvaldo Sala, Arizona State University Berkeley Edward “Ted” Schuur, Northern Arizona Jonathan Bamber, University of Bristol University Barbara A. Bekins, U.S. Geological Survey Sybil Seitzinger, University of Victoria Jayne Belnap, Southwest Biological Science Toshihiko Shimamoto, Institute of Geology, Center, U.S. Geological Survey China Earthquake Administration Thomas S. Bianchi, University of Florida Adam Showman, University of Arizona Jean Braun, GFZ Helmholtz Centre Potsdam, V. Sobolev, Institut des Sciences and Institute of Earth and Environmental de la Terre, Université Grenoble Alpes, Sciences, University of Potsdam and Vernadsky Institute of Geochemistry Ximing Cai, University of Illinois at ­Urbana-​ Joseph R. Dwyer, University of New and Analytical Chemistry, Russian Academy Champaign­ Hampshire of Sciences Ken Carslaw, James Farquhar, University of Maryland, Carl Steefel, Lawrence Berkeley National Benjamin F. Chao, Institute of Earth Sciences, College Park Laboratory Academia Sinica Mei-Ching Fok, NASA Goddard Space Flight John Suppe, University of Houston Patrick Cordier, Université de Lille Center Karl E. Taylor, Lawrence Livermore National Rosanne D’Arrigo, Lamont-Doherty Earth Piers Forster, University of Leeds Laboratory Observatory of Columbia University Christian -Lanord, CNRS Université Meenakshi Wadhwa, Arizona State University Eric A. Davidson, Appalachian Laboratory, de Lorraine Michael Walter, Carnegie Institution University of Maryland Center for Antoinette B. Galvin, University of New for Science Environmental Science Hampshire John Wettlaufer, Yale University and Nordic Gert J. de Lange, Utrecht University Peter R. Gent, National Center for Institute for Theoretical Physics Andrew Dessler, Texas A&M University Atmospheric Research Chunmiao Zheng, Southern University of Michele K. Dougherty, Imperial College Taras Gerya, ETH Zurich Science and Technology, Shenzhen London Dennis Hansell, University of Miami Tong Zhu, Peking University

38 // Eos October 2019 AGU NEWS

Alik Ismail-Zadeh, Karlsruhe Institute 2019 AGU Union Medal, Award, of Technology Margaret Leinen, Scripps Institution and Prize Recipients Announced of Oceanography Constance Millar, Pacific Southwest Research Station, U.S. Forest Service Lixin Wu, Ocean University of China ach year, AGU honors individuals for their outstanding achievements, contributions, and Edward A. Flinn III Award service to the Earth and space science community. AGU medals are the highest honors James Broda, Woods Hole Oceanographic E bestowed by the Union. In this, AGU’s Centennial year, when we commemorate the past Institution and look to the future, we recognize individuals for their body of scientific work and sustained Athelstan Spilhaus Award impact within the Earth and space science community. AGU Union awards and prizes recognize Brian May, Commander of the Most Excellent individuals who have demonstrated excellence in scientific research, education, communication, Order of the British Empire (CBE) and outreach. International Award This distinguished group of honorees—scientists, leaders, educators, journalists, and com- Susan Elizabeth Hough, U.S. Geological municators—embodies AGU’s mission of promoting discovery in Earth and space science for the Survey benefit of humanity. Excellence in Earth and Space Science On behalf of AGU’s Honors and Recognition Committee, the selection committees, and AGU Education Award leaders and staff, we are pleased to present the recipients of AGU’s 2019 Union medals, awards, David J. P. Moore, University of Arizona and prizes and honor the important role they play in amplifying the voice of the Earth and space Africa Award for Research Excellence community while inspiring other scientists to help improve lives around the world. in Ocean Sciences We appreciate everyone who has shown support and commitment to AGU’s Honors Program. Andrew Green, University of ­KwaZulu-Natal​­ Our dedicated volunteers gave valuable time as members of selection committees to choose this Africa Award for Research Excellence year’s Union medal, award, and prize recipients. We also thank all the nominators and support- in Space Science ers who made this possible through their steadfast efforts to nominate and recognize their col- Andrew Akala, University of Lagos leagues. Science for Solutions Award Franziska C. Landes, Lamont-Doherty Celebrate at Fall Meeting Earth Observatory of Columbia University We look forward to celebrating our honorees’ profound contributions at this year’s Honors Cere- Robert C. Cowen Award for Sustained mony and Banquet, to be held Wednesday, 11 December, at Fall Meeting 2019 in San Francisco, Achievement in Science Journalism Calif. Alexandra Witze, Freelance Please join us in congratulating our esteemed class of 2019 Union honorees listed below. Walter Sullivan Award for Excellence in Science Journalism Sarah Kaplan, The Washington Post By Robin Bell, President, AGU; and Mary Anne Holmes ([email protected]), Chair, Honors David Perlman Award for Excellence and Recognition Committee, AGU in Science Journalism Ann Gibbons, Contributing Correspondent, Science Medals Robert E. Horton Medal Spilhaus Ambassador Award Grant S. Majid Hassanizadeh, Utrecht University Esteban Gabriel Jobbágy, National Barbara A. Romanowicz, University of Harry H. Hess Medal Scientific and Technical Research Council California, Berkeley; Collège de France; Richard J. Walker, University of Maryland, (CONICET) and Universidad Nacional and Institut de Physique du Globe College Park de San Luis de Paris Michael Edward Wysession, Washington James B. Macelwane Medal , University of Maryland, University in St. Louis Amir AghaKouchak, University College Park of California, Irvine Prizes Anton Artemyev, University of California, Ulrich R. Christensen, Max Planck Institute Asahiko Taira International Scientific Los Angeles for Solar System Research Ocean Drilling Research Prize Emily V. , Colorado State University Joanne Simpson Medal for Mid-Career Scientists Beth N. Orcutt, Bigelow Laboratory Francis A. Macdonald, University Penelope L. King, Australian National for Ocean Sciences of California, Santa Barbara University Climate Communication Prize Erik van Sebille, Utrecht University Ann Pearson, Harvard University Marshall Shepherd, University John Adam Medal Fuqing Zhang, Pennsylvania State University of Georgia Michelle F. Thomsen, Planetary Science Devendra Lal Memorial Medal Institute Kuljeet Kaur Marhas, Physical Research Walter H. Bucher Medal Laboratory Leigh Royden, Massachusetts Institute Sign Up for Eos Buzz of Technology Awards Medal Ambassador Award at bit.ly/Eos-Buzz Maureen E. Raymo, Lamont-Doherty Sunanda Basu, National Science Foundation Earth Observatory of Columbia University (Ret.)

Earth & Space Science News Eos.org // 39 RESEARCH SPOTLIGHT

Forested Streams May Warm More Than Observations Predict

Forested streams in maritime climates are getting warmer, posing hazards for cold-­ water​­ fish like salmon. Credit: Bonnie Moreland, CC0 1.0 (bit.ly/ccby1-0)

s average air temperatures rise, the temperatures of forested The researchers used their model to generate simulated streamflows streams that provide key habitats for salmon and other cold-­ ​ and temperatures for a 51-­ year​­ historic period as well as several future A ­water organisms typically rise as well, but the relationship climate change scenarios, such as an increase in air temperature of 2°C. isn’t necessarily straightforward. New research suggests that these They ran the model for two elevation zones—one dominated by rain streams may warm even more in the future than some models have and the other with significant snowmelt contributions—and with four predicted. different values for the fraction of soil water that ends up discharging Clarifying exactly how climatic warming affects stream temperatures as groundwater into the stream. is important for understanding and potentially managing negative eco- The simulations revealed that stream temperatures may be up to system impacts. Previous research has suggested that empirical models twice as sensitive to climate change as predicted by ­observation-based​­ relying purely on observed relationships between air and stream tem- models. The analysis suggests that empirical models do not adequately peratures tend to underpredict future stream warming compared with account for future effects of global warming on key processes, such as computational models that incorporate physical processes. reductions in winter snow cover and reductions in plant shade. It also To sort out the discrepancies between the different types of models, suggests that streams fed by groundwater may resist warming in the Leach and Moore drew on work they performed in the Malcolm Knapp near term but will eventually warm as groundwater temperatures rise. Research Forest near Vancouver, B.C., Canada. They used numerous The findings highlight the importance of considering prior condi- field measurements to build and calibrate a ­process-based​­ model tions when evaluating how sensitive ­cold-water​­ streams are to climate incorporating several key factors, such as tree canopy cover, snowmelt, change and, ultimately, how aquatic ecosystems will be affected. The and groundwater discharge. The model simulates daily streamflow and authors call for a shift from purely empirical modeling methods to temperature for virtual streams that are representative of forested approaches that better account for key feedbacks that affect stream streams in maritime climates, such as those found in northwestern temperature sensitivity. (Water Resources Research, https://doi​ .​ org/­ 10​ ​ North America. .1029/2018WR024236,­ 2019) —Sarah Stanley, Freelance Writer

40 // Eos October 2019 RESEARCH SPOTLIGHT

Variations in Creep Along One of Earth’s Most Active Faults

s part of the earthquake cycle, most earthquakes since 1939. The most recent The team also presented evidence for a active faults suddenly release strain event, the 1999 magnitude 7.4 Izmit earth- transient “creep burst” that occurred along A that has gradually accumulated for quake that occurred roughly 100 kilometers the same fault segment in November 2016. extended periods of time. Some faults, how- east of Istanbul, ruptured five segments and During this spike, the surface slip totaled ever, may experience aseismic slip, or creep, killed more than 20,000 people. 10 millimeters, a distance that corresponds to which sometimes begins after a major seis- Using 307 images acquired by the 1.25 years of average creep, in just 3 weeks. mic event and then steadily declines over Sentinel-1 and TerraSAR- X satellites, the Collectively, these findings indicate that time. Determining the relative proportion of researchers examined ground velocity postseismic slip along the North Anatolian seismic and aseismic slip occurring along an changes in space and time across the central Fault is more complex than has previously active fault is critical for accurately estimat- segment of the 1999 rupture for the period been suggested. By providing evidence that ing its potential seismic hazard. spanning 2011–2017. The results indicate that creep is not necessarily a steady process, this In a new study, Aslan et al. use recent, high- this segment continues to creep nearly study offers new insight into long- term, resolution interferometric synthetic aperture 2 decades after the earthquake but that its postseismic deformation following a major radar data to characterize aseismic slip occur- maximum rate in the fault- parallel horizon- earthquake along one of Earth’s most active ring along Turkey’s North Anatolian Fault, the tal direction has tapered to an average of strike- slip faults. ( Journal of Geophysical 1,600- kilometer- long strike- slip feature sep- roughly 8 millimeters per year, about two Research: Solid Earth, https:// doi . org/ 10 . 1029/ arating the Eurasian and Arabian plates that thirds the rate measured during the previous 2018JB017022, 2019) —Terri Cook, Freelance has produced seven large (magnitude > 7) decade. Writer

A Better Way to Measure Cloud Composition

he effects of clouds on Earth’s climate are so complex that some scientists have called them the wild card of climate science. T Clouds can either cool Earth’s surface by reflecting sunlight or trap heat like a blanket, leaving scientists unsure of whether clouds will accelerate or slow global warming. To understand the relationship between clouds and climate, researchers are scrambling to better measure and model clouds’ ever changing qualities, such as the sizes of the tiny ice particles and water droplets that compose them. Jiang et al. propose a new method to measure cloud properties from space more accurately, which could improve climate and weather pre- dictions. The researchers combined two types of remote sensing tech- nology—active and passive sensors—to create an instrument suite that can accurately capture many different properties of clouds at high reso- lution. Active sensors shoot beams of microwaves at clouds and use the echoed signals to study their composition, whereas passive sensors detect various wavelengths of electromagnetic radiation emitted by clouds themselves. The new tool builds on an existing instrument called Tropospheric Water and Cloud ICE (TWICE), which detects 14 different millimeter and submillimeter wavelengths and which Jiang and colleagues have described in previous studies. The new instrument, called Earth’s Next- Researchers are developing new methods to better understand the composition of generation ICE (ENTICE), adds two more frequencies: 94 gigahertz for clouds, including wispy cirrus clouds like those pictured here, and their impact on cli- active radar detection and 850 gigahertz for use in a passive radiometer. mate and weather. Credit: PiccoloNamek, CC BY-SA 3.0 (bit.ly/ccbysa3-0) The added frequencies improve the vertical resolution of ice cloud mea- surements from 3– 4 kilometers to 0.5 kilometer, the team reports. The combined 94- gigahertz radar and multifrequency radiometer standing the dynamic and small- scale processes that occur within suite also enabled ENTICE to more accurately capture the effective clouds and could improve both climate models and weather forecasts, diameters of ice particles within clouds while simultaneously measur- the team says. (Earth and Space Science, https://doi . org/ 10 . 1029/ ing humidity and temperature. Such measurements are key to under- 2019EA000580, 2019) —Emily Underwood, Freelance Writer

Earth & Space Science News Eos.org // 41 RESEARCH SPOTLIGHT

New Perspectives on 2,000 Years of North Atlantic Climate Change

A new review paper explores recent progress in research addressing the potential role of North Atlantic Ocean circulation in historical climate shifts over the past 2 millennia. Credit: Brocken Inaglory, CC BY-­ SA 3.0​­ (bit.ly/ccbysa3-0)

istorical and natural clues suggest that Earth’s climate under- fields: observational data that provide proxy clues to past oceanic and went small changes over the past 2,000 years, and variations climate conditions, such as cores and the remains of shelled H in North Atlantic Ocean circulation may have been a key organisms, and models that simulate the past climate. driver. In a new paper, ­Moffa-​­Sánchez et al. compile recent advance- The authors unite a number of previously published proxy data sets ments in ­analytical tools used to probe this period of ocean circula- to paint a picture of North Atlantic Ocean circulation over the past tion, presenting a comprehensive overview of current knowledge. 2,000 years. This compilation reveals details of past conditions in var- The past 2 millennia have seen several ­centuries-​­long climate ious regions. For example, the past 2,000 years around Greenland shifts, such as the Medieval Warm Period, followed by the Little Ice show progressively cooler and icier surface waters reaching the cold- Age, which were particularly recorded around the North Atlantic. The est conditions during the Little Ice Age. The compilation also under- North Atlantic is an important climatological region because of the scores a need for more comprehensive data sets on deep North Atlan- strong interactions between ocean, atmosphere, and sea ice, as well as tic waters for this period. the overturning circulation between surface and deep-­ ​­ocean currents. To gain further insight, the authors selected and compared three Scientists have traditionally proposed that changes in this Atlantic recently developed climate models that are particularly well suited for Meridional Overturning Circulation played a key role in the observed studying the North Atlantic’s past climate over the past millennium. climate shifts, but this view remains under debate because of the lack They identified key areas of uncertainty and disagreement between of clear evidence. the models that could be addressed in future research. They also The new review synthesizes 20 years’ worth of rapid progress demonstrated agreement between model and proxy data estimates of toward understanding the role of ocean circulation in historical cli- sea surface temperatures for some historical periods and regions but mate change. The authors highlight advancements in two major disagreement for others. These findings highlight important advancements toward under- standing how changes in ocean circulation may have affected historical u Read the full stories climate change while emphasizing areas for improvement. The authors note the promise of using models to fill gaps in observational data but and the latest breaking news also call for continued collection and improvement of proxy data sets. at Eos.org (Paleoceanography and Paleoclimatology, https://doi​ .​ org/­ 10​ .​ 1029/­ ​ 2018PA003508, 2019) —Sarah Stanley, Freelance Writer

42 // Eos October 2019 RESEARCH SPOTLIGHT

Déjà Vu: Understanding Subduction Zones’ Cycle of Seismicity

long the southeastern edge of Japan’s record a complete, postseismic Honshu Island, the Philippine Sea phase is in southern Japan, A plate is diving beneath the Eurasian where leveling surveys as well as plate at the Nankai subduction zone. Seismic- and GPS measure- ity there has unleashed numerous devastat- ments collectively span the ing, megathrust earthquakes in a cycle typi- period from 1890 to the present. cally characterized by pairs of closely spaced Johnson and Tebo have harnessed tremors that have occurred every 146 years, on this unique data set to model average, since 1361. The region’s most recent vertical deformation in the Nan- earthquakes were the magnitude 8.1 Tonankai kai region from 1947 to 2015. and the magnitude 8.4 Nankai events, which The results indicate that fol- occurred in 1944 and 1946, respectively. lowing the 1940s earthquakes, The seismic cycle is the process of repeat- subsidence was centered about edly building stress on a fault over a long 250 kilometers inland of the period of time that is rapidly released in a large Nankai trench, and its rate grad- This map shows vertical motions in southwestern Japan 7 years after the earthquake. Previous studies have recognized ually decreased from 1947 until . Credit: Kaj Johnson that mantle flow plays a crucial role in the approximately 1995. By contrast, seismic cycle by relaxing postseismic stresses postseismic uplift occurred as well as straining the fault during the inter- within a narrow belt stretching along Hon- on the order of 1019 pascal seconds, which seismic buildup to the next tremor. The sur- shu’s southeastern coast, but it slowed and corresponds to a mantle relaxation time of face deformation that accompanies this cycle then switched to subsidence by the mid- 5–15 years. As the first study to clearly cap- can vary considerably depending on the man- 1960s. ture 5 decades of postseismic mantle flow, tle’s viscosity. But inferring this parameter According to the authors’ two- dimensional this research offers a crucial contribution to has proven difficult because of a lack of geo- modeling results, the uplift is best explained improving our understanding of the cycle of detic data sets that span the centuries- long by afterslip along the coast, whereas the seismicity that occurs in Earth’s subduction timescales of most seismic cycles. inland subsidence is strongly indicative of zones. ( Journal of Geophysical Research: Solid The only place in the world where a record postseismic flow within the . Earth, https:// doi . org/ 10. 1029/ 2018JB016345, exists that is long enough to potentially The best fit to this pattern requires a viscosity 2018) — Terri Cook, Freelance Writer

Demystifying Sea Level Changes Along the New England Coast

he Atlantic Meridional Overturning Now Piecuch et al. are challenging the con- England sea level change are instead related Circulation (AMOC), a system of cur- ventional wisdom that a direct causal con- to the North Atlantic Oscillation and other T rents in the Atlantic Ocean that trans- nection exists between the AMOC and coastal surface atmospheric variations. ports warm surface waters northward and sea level in this region. After obtaining Although this study represents a valuable cooler, deeper waters southward, is a monthly RAPID monitoring program obser- contribution to improving our understanding crucial component of Earth’s climate sys- vations of the overturning circulation at 26°N of how coastal sea level is related to oceanic tem. Because the AMOC is part of a conveyor and monthly sea level records collected circulation, the authors caution that their belt of oceanic circulation that redistributes between 2004 and 2017 at eight New England results apply only to the time period studied heat around the globe, variability in its tide gauges, they examined the physical rela- and that the negative correlation between strength can have significant climate conse- tionships between the two records. coastal sea level and overturning at 26°N quences. The authors conclude that widespread should not be considered representative of Previous modeling studies have concluded atmospheric teleconnections can simultane- the AMOC at other latitudes. They suggest that the AMOC’s strength is negatively cor- ously trigger changes in both the AMOC at that future studies could shed new light on related to sea level along the New England 26°N and coastal New England sea level. the processes occurring at higher latitudes, coastline, such that a weakening of the North Although these phenomena are temporally where new AMOC monitoring arrays have Atlantic Current or the leads to a correlated with each other, they conclude recently been established. (Geophysical rise in sea level at the coast. This relation- that they are not causally linked. The Research Letters, https:// doi . org/ 10 . 1029/ ship, however, has been difficult to detect in researchers argue that the local atmospheric 2019GL083073, 2019) —Terri Cook, Freelance observational records. forcing mechanisms driving coastal New Writer

Earth & Space Science News Eos.org // 43 POSITIONS AVAILABLE

Hydrology required at the time of appointment, with the position scheduled to begin The Career Center (findajob.agu.org) Assistant Professor in Hydrology & in Fall 2020, subject to budgetary Water Sustainability approval. Please apply online to: is AGU’s main resource for recruitment The Department of Geology and https://facultysearch​­ .​ as­ .​ pitt­ .​ edu/­ ​ Environmental Science at the Uni- apply/­ index/​­ MjY4.​­ Applications advertising. versity of Pittsburgh invites applica- should include: 1) cover letter; 2) CV; tions for a ­tenure-track​­ assistant 3) research statement; 4) research professor position in Hydrology and statement; 5) diversity statement; AGU offers online and printed recruitment Water Sustainability. 6) four references; and 7) copies of We are seeking a geoscientist who three relevant publications. Please advertising in Eos to reinforce your characterizes hydrologic change and direct questions to the Search Com- evaluates adaptation strategies for mittee Chair, Dr. Daniel Bain, online job visibility and your brand. Visit sustainable adjustment to these dbain@pitt.​ edu,­ 412-­ 624-​­ 8766.​­ changes. This colleague ideally uses Information about the University employers.agu.org for more information. combinations of field measurements of Pittsburgh can be found at https://​ and observations, modeling, and/or www.​ hr­ .​ pitt­ .​ edu/­ why​­ -​ work­ -​ pitt.­ For remote sensing to better understand information on the University of water-­ climate-​­ human​­ interactions. Pittsburgh’s generous package of The successful candidate will benefits, visit http://www​­ .​ hr­ .​ pitt­ ​ Packages are available for positions that are establish an externally-­ funded,​­ .edu/­ benefits.​­ internationally recognized research Pitt is an EEO/AA/M/F/Vets/Dis- program that complements existing abled employer. Full advertisement: • SIMPLE TO RECRUIT Department strengths. In particular, https://www​ .​ geology­ .​ pitt­ .​ edu/­ news/​­ ​ u online packages to access our Career Center audience the Department hosts the Collabora- assistant­ -​ professor­ -​ hydrology­ ​ tory for Water Research, Education, -water­ -​ sustainability­ u 30-day and 60-day options available and Outreach (https://www​ .​ water­ ​ .­pitt​.­edu) and the University Climate Earth Research Scientist (career-­ ​ u prices range $475–$1,215 and Global Change Center (https://​ track)­ www.​ climatecenter­ .​ pitt­ .​ edu/),­ both Berkeley Lab’s Earth and Environ- platforms for cutting edge, interdis- mental Sciences Area has an opening • CHALLENGING TO RECRUIT ciplinary water science. Teaching for a Research Scientist in Integrated duties include undergraduate and Hydrological Modeling. In this posi- u online and print packages to access the wider AGU community graduate courses in the candidate’s tion, you will be expected to work on area of expertise. a wide variety of integrated hydrol- u 30-day and 60-day options available Review of applicants will begin on ogy problems related to water quan- October 15, 2019 and continue until tity and quality and to employ a u prices range $795–$2,691 the position is filled. A PhD is range of tools from ­data-​­driven to • DIFFICULT TO RECRUIT u our most powerful packages for maximum multimedia exposure to the AGU community

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44 // Eos October 2019 POSITIONS AVAILABLE

mechanistic models, and a combina- • Collaborate with and/or lead oth- tion of them, with consideration of ers in groups and forge/lead collabora- the appropriate climate drivers. tions across the Area, Lab and with What You Will Do: colleagues at external institutions. • Develop and use models to How To Apply understand hydrological response to Apply directly online at http://​­50​.­73​ perturbations at multiple scales, .­55​.­13/​­counter.​ ­php?id=167292 and fol- from the global to the regional to the low the ­on-​­line instructions to com- watershed scale. plete the application process. • Combine data-­ driven,​­ machine-­ ​ ­learning and mechanistic modeling Interdisciplinary approaches to advance understand- ing of integrated hydrology problems Assistant Professor of Earth and affected by evolving climate forc- Environmental Sciences ings. The Department of Earth and Envi- • Analyze and integrate complex ronmental Sciences in the College of datasets including high-­ resolution​­ Liberal Arts and Sciences at the Uni- climate data and distributed hydro- versity of Illinois at Chicago (UIC) logical measurements. invites applications for a ­tenure-track​­ • Use weather forecasting and cli- Assistant Professor who pursues fun- mate models to drive mechanistic damental research in climate science integrated hydrological models, sub- with an emphasis on surface pro- setting results where needed. cesses. The applicant’s research • Use a variety of computational should involve more than one codes available in the Department of approach (e.g., observational, model- Energy software ecosystem that sim- ing, experimental) and may address ulate overland and/or subsurface topics that include, but are not limited flow and reactive transport. to, the effects of climate change on • Develop new research areas and biogeochemical cycling and the role of proposals. climate in landscape evolution. The • Conduct innovative research successful candidate is expected to and publish in ­peer-​­reviewed and establish an innovative and productive high impact journals program of scientific research that • Regularly present findings at complements department strengths in major conferences and workshops ecohydrology, planetary science, and • Contribute to Lab and Commu- , and can contribute nity Professional Service, and lead/ to university strengths in areas such organize workshops/meetings. as public health. The candidate will

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Earth & Space Science News Eos.org // 45 POSITIONS AVAILABLE

teach graduate and undergraduate in compliance with the Fair Credit research and education, and in inter- ties, women, protected veterans and courses, advise graduate students (MS Reporting Act. actions with the community. The Dep- individuals with disabilities. Miami and PhD), and mentor undergraduate uty Division Director assumes the University prohibits harassment, dis- students in research projects. Appli- Deputy Division Director for the Divi- Division Director’s role in the absence crimination and retaliation on the cants must have a PhD in Earth Sci- sion of Astronomical Sciences (AST) of the Division Director. basis of sex/gender (including sexual ences or a related field, and a record of Serves as Deputy Division Director Apply via email at execsrch@nsf​.gov­ harassment, sexual violence, sexual research accomplishments; postdoc- for the Division of Astronomical Sci- misconduct, domestic violence, dating toral experience is preferred. ences (AST) in the Directorate for Assistant Lecturer/Assistant Teach- violence, or stalking), race, color, reli- The Earth and Environmental Sci- Mathematical and Physical Sciences. ing Professor gion, national origin (ancestry), dis- ences Department (https://​­eaes​.­uic​ The Division contributes to NSF’s The Department of Geology and ability, age (40 years or older), sexual .­edu/) has extensive laboratory and mission by supporting research in all Environmental Earth Science at Miami orientation, gender identity, preg- computing facilities, and is expanding areas of astronomy and astrophysics University invites applications for a nancy, status as a parent or par- collaborations with other campus and related multidisciplinary studies. ­full-time​­ Assistant Lecturer or Assis- ent, military status, or veteran status units including chemistry, health sci- Modes of support include ­single-​ tant Teaching Professor position on in its recruitment, selection, and ences, and biological sciences. The ­investigator and collaborative awards, the Oxford campus, beginning August employment practices. Requests for Department serves a growing body of construction, operations, and mainte- 2020. The Assistant Lecturer/Assis- all reasonable accommodations for majors, the majority of whom are nance of national observatories, as tant Teaching Professor will teach disabilities related to employment underrepresented in STEM. UIC is a well as funding for acquisition and undergraduate courses, including should be directed to ADAFacultyStaff@­ ​ public R1 institution and one of the development of astronomical instru- foundation courses in physical and ­miamioh​.­edu or ­513-​­529-​­3560. most ethnically and culturally diverse mentation, technology development environmental geology, as well as As part of the University’s commit- universities in the country. It is the and future ­ground-based​­ facilities, intermediate level courses; advise ment to maintaining a healthy and safe largest institution of higher education and education projects that leverage undergraduate students; and provide living, learning, and working environ- in the Chicago area with over 30,000 the Division’s research investments to professional service to the department ment, we encourage you to read Miami undergraduate, graduate, and profes- build research and workforce capacity and university. Required: M.S. in geo- University’s Annual Security & Fire sional students. To apply, please com- and to increase scientific literacy. science (for appointment as Assistant Safety Report at http://www​.miamioh­ ​ plete the online application providing Through the national observatories, Lecturer) or Ph.D. in geoscience (for .edu/­ campus​­ -​ safety/­ annual​­ -​ report/­ ​ contact information and three profes- including international partnerships, appointment as Assistant Teaching ­index​.­html, which contains informa- sional references at https://jobs.​­uic​ the Division provides support for a Professor) by time of appointment, tion about campus safety, crime sta- .­edu (click on the Job Board and then system of ­multi-​­aperture, ­research-​ and documented teaching experience; tistics, and our drug and alcohol abuse on the position link) and upload a ­class telescopes as well as frontier applicant must be a U.S. citizen, a and prevention program designed to cover letter, curriculum vitae, and facilities that enable transformational lawful permanent resident, admitted prevent the unlawful possession, use, statements of research and teaching capabilities in both radio and optical/ for residence as an applicant under the and distribution of drugs and alcohol plans. For fullest consideration, please infrared astronomy. Within the Divi- 1986 immigration amnesty law, refu- on campus and at university events apply by October 21, 2019. Final sion, the Deputy Division Director gee or asylee. Desired: interest in con- and activities. This report also con- authorization of the position is subject works with the Division Director in tributing to supervision of undergrad- tains information on programs and to availability of funding. The Univer- providing leadership and management uate student research and field-­ ​­based policies designed to prevent and sity of Illinois at Chicago is an affir- to the Division’s programs and assists experiences. Submit letter of applica- address sexual violence, domestic mative action, equal opportunity the Division Director in carrying out tion, curriculum vitae, and evidence of ­violence, dating violence, and employer, dedicated to the goal of ­Division-​­wide responsibilities such as teaching effectiveness to http://​jobs​ stalking. Each year, email notification building a culturally diverse and plu- the preparation of budget submissions .­miamioh​.­edu/​­cw/​­en​-­us/​job/​495551. of this website is made to all faculty, ralistic faculty and staff committed to for Congress, oversight and manage- Letters of reference will be requested staff, and enrolled students. Written teaching and working in a multicul- ment of the Division budgets, and the upon receipt of application. Inquiries notification is also provided to pro- tural environment. We strongly recruitment of scientific staff. The can be directed to Cathy Edwards at spective students and employees. encourage applications from women, incumbent also supervises and pro- edwardca@miamioh​ ​.­edu. Review of Hard copies of the Annual Security & minorities, individuals with disabili- vides leadership and guidance to applications will begin on October 2, Fire Safety Report may be obtained ties and covered veterans. The Univer- administrative and support personnel 2019 and continue until position is from the Miami University Police sity of Illinois may conduct back- within the Division. Externally, the filled. Department at (513) ­529-​­2225. Crimi- ground checks on all job candidates Deputy Division Director represents Miami University, an Equal Oppor- nal background check required. All upon acceptance of a contingent offer. the Division in a variety of ­NSF-​­wide tunity/Affirmative Action employer, campuses are ­smoke- and ­tobacco-​ Background checks will be performed and interagency activities related to encourages applications from minori- ­free.

46 // Eos October 2019 POSITIONS AVAILABLE

Research Positions to investigate status, protected veteran status, or Lagrangian ­sea-​­ice model will be used sity service. We seek candidates who new approaches to modeling plane- any other characteristic protected by to study the large-­ ​­scale properties of will strengthen existing research pro- tary boundary layers and law. sea ice, which are emergent from indi- grams in planetary science and remote in Earth system models vidual floe interactions. sensing, as well as foster collaboration The Atmospheric and Oceanic Sci- Director, Electron Microbeam Labo- The ideal candidate has a strong with scholars across the Washington ences program at Princeton Univer- ratory, University of ­Wisconsin-​ background in one or more areas University community. sity, in cooperation with NOAA’s Geo- Madison­ among ­sea-​­ice dynamics, material Candidates must have a Ph.D. in physical Fluid Dynamics Laboratory The Department of Geoscience at science, geophysical fluid dynamics, planetary science or a related field at (GFDL), seeks postdoctoral or more the University of ­Wisconsin-​­Madison ­soft-matter​­ science, and numerical the time of appointment. In addition, senior researchers for new projects on invites applications at the Assistant, methods. Experience with scientific candidates at the associate or full pro- modeling planetary boundary layers Associate, or Senior Scientist level to software development, Lagrangian fessor rank must have an advanced and convection in Earth system mod- fill the Director’s position in the methods, ­discrete-​­element methods record of research, publication, and els at GFDL, particularly for (1) imple- Eugene Electron Microprobe or smoothed particle hydrodynamics teaching warranting tenure. Complete menting and analyzing an diffu- Laboratory (http://www​.­geology​.­wisc​ solvers will be advantageous in this applications include cover letter, cur- sivity/mass flux (EDMF) .­edu/​~­johnf/​­sx51.​ ­html). This is a ­full-​ research. riculum vitae, statements of teaching parameterization for boundary layers ­time, ­institutionally-supported​­ posi- Candidates must have a Ph.D. in and research interests, and names and and convection and (2) improved tion with competitive salary. The lab either applied mathematics, physics, contact information of at least four modeling of momentum flux in plane- houses SX51 and SX5FE electron cryosphere, or a related field. Initial references, submitted via Interfolio: tary boundary layers. The first project microprobes, a Hitachi S3400 VP scan- appointment is for one year with the https://​­apply​.­interfolio​.­com/​­66099. is a collaboration with the Jet Propul- ning electron microscope, and a lab possibility of renewal subject to satis- Applications must be received by sion Laboratory. The researcher will manager to assist with SEM mainte- factory performance and available October 31, 2019 to ensure consider- work in collaboration with GFDL, nance and operations. The lab serves funding. ation. UCLA, The University of , as a hub for interdisciplinary scientific Complete applications, including a Washington University in St. Louis and the National Center for Atmo- inquiry, providing ­hands-on​­ training CV, publication list, a statement of is committed to the principles and spheric Research, aiming at a unified of students from disciplines across research interests, and contact infor- practices of equal employment oppor- approach to moist turbulent processes campus. Additional departmental mation of 3 references should be sub- tunity and especially encourages for boundary layers and deep convec- resources include two electronics mitted by September 15, 2019 for full applications by those underrepre- tion. The second project is a collabora- engineers and a staffed ­thin-​­section consideration. Applicants should sented in their academic fields. It is tion with the Pennsylvania State Uni- lab. Applicants should hold a Ph.D. in apply online https://​www​.­princeton​ the University’s policy to recruit, hire, versity. The researcher will work in Earth Sciences, Chemistry, Physics, .­edu/​acad​-­positions/​­position/​­12908. train, and promote persons in all job collaboration with GFDL, Penn State, Material Science, or related fields at For more information about the titles without regard to race, color, and the National Center for Atmo- time of appointment. Demonstrated research project and application pro- age, religion, sex, sexual orientation, spheric Research, aiming at including ability and experience in the use of cess, please contact Alistair Adcroft gender identity or expression, national momentum flux in ­higher-​­order clo- electron beam instruments for high-­ ​ (aadcroft@princeton​ ​.­edu) and Olga origin, protected veteran status, dis- sure for ­boundary-layer​­ turbulence. ­quality, quantitative analyses is Sergienko (osergien@​­princeton​.­edu). ability, or genetic information. The positions support newly funded, required. Two or more years of daily This position is subject to the Uni- ­multi-​­agency, interdisciplinary Cli- ­hands-on​­ management of an electron versity’s background check policy. Seismology mate Process Teams. The teams will microprobe lab is preferred, as is Princeton University is an equal provide opportunities to blend model- demonstrated ability to pursue fund- opportunity employer and all qualified Postdoctoral or more Senior ing, theory, and observational per- able research using electron applicants will receive consideration Researcher, Department of Geosci- spectives. The Climate Process Teams microbeam instrumentation. Appli- for employment without regard to ences at Princeton University are tackling some of the most chal- cants should submit the following: race, color, religion, sex, national ori- The Theoretical & Computational lenging problems in climate science (1) cover letter that includes your gin, disability status, protected vet- Seismology group in the Department and atmospheric prediction using one research statement, (2) curriculum eran status, or any other characteristic of Geosciences at Princeton Univer- of the world’s leading modeling sys- vitae, and (3) the names and contact protected by law. sity, led by Professor Jeroen Tromp, tems. information for three referees. Please has an opening for a postdoctoral or Successful applicants will work apply by October 15, 2019 to guarantee Planetary Sciences more senior researcher. Essential with Leo and Ming Zhao at full consideration, although applica- qualifications include a Ph.D. in Geo- GFDL and ­multi-​­institutional team tions will continue to be accepted until Professor of Earth and Planetary Sci- sciences or related field and excellent members. the position is filled. For more infor- ences computational skills. The research will Scientists with backgrounds in gen- mation and to apply, go to: https:// The Department of Earth and Plan- focus on seismic full waveform inver- eral circulation modeling, parameter- jobs​.­hr.​ ­wisc.​ ­edu/​­en​-­us/​job/​­502003/​ etary Sciences at Washington Univer- sion of ­controlled-source​­ data to ization development, and modeling of ­epma​-­lab​-­director sity in St. Louis invites applications determine shallow heterogeneities atmospheric processes are especially for a ­tenure-track​­ or tenured faculty and voids. The position is available for encouraged to apply. Candidates must Ocean Sciences position at the assistant, associate, or one year, with a possibility for renewal have a PhD in atmospheric science or full professor rank, commensurate contingent upon satisfactory perfor- a related field. Complete applications, Postdoctoral Research Scientist in with experience, in the field of plane- mance and funding. including a CV, a statement describing Lagrangian Sea-­ Ice​­ Modelling tary science. The candidate is expected Applicants should include a cover research interests and how they would The Atmospheric and Oceanic Sci- to perform research in the broad area letter, a curriculum vitae including a contribute to the project, and contact ences Program and the Andlinger of planetary surfaces and processes, publication list, and contact informa- information for 3 references should be Center for Energy and the Environ- have or seek active involvement in tion for three references and must submitted by September 15, 2019 for ment at Princeton University, in asso- planetary science missions, and even- apply via the Princeton University full consideration. Applicants should ciation with NOAA’s Geophysical Fluid tually assume leadership of the NASA Academic Hiring website https://www​ apply online to http://www​.­princeton​ Dynamics Laboratory (GFDL), seeks a Planetary Data System Geosciences .­princeton​.­edu/​­acad​-­positions/​ .­edu/​­acad​-­positions/​­position/​­13141. postdoctoral or more senior researcher Node at Washington University. The ­position/​­13161. This position is sub- For more information about the to develop a Lagrangian model of ­sea-​ ideal candidate will employ quantita- ject to the University’s background research projects and application pro- ­ice dynamics for use in regional and tive tools and will integrate computa- check policy. Princeton University is cess, please contact Leo Donner (­leo.j​ global ocean circulation models. tional approaches with remotely an equal opportunity employer/affir- .­donner@noaa.​ ­gov) or Ming Zhao This work will involve exploring sensed observations. mative action employer and all quali- (ming​.­zhao@noaa.​ ­gov). This position innovative approaches to modeling The successful candidate is fied applicants will receive consider- is subject to the University’s back- sea ice, with a focus on representing expected to develop a vigorous, exter- ation for employment without regard ground check policy. Princeton Uni- sea ice floes, and collections of floes, nally funded research program, main- to age, race, color, religion, sex, sex- versity is an equal opportunity as Lagrangian elements. The project tain a strong publication record, ual orientation, gender identity or employer and all qualified applicants aims to construct an operational advise students, provide outstanding expression, national origin, disability will receive consideration for employ- Lagrangian ­sea-​­ice model, which can teaching of undergraduate and gradu- status, protected veteran status, or ment without regard to race, color, be tested against existing ­grid-​­based ate courses, and participate actively in any other characteristic protected by religion, sex, national origin, disability numerical models of sea-­ ​­ice. The departmental governance and univer- law.

Earth & Space Science News Eos.org // 47 POSTCARDS FROM THE FIELD

Greetings from near Shreveport, Louisiana!

This is one of the very first field shots from the Investigation seismic waves from the distant 4 July M6.4 and 6 July M7.1 of Seismicity in Louisiana (ISLA) project backdropped against earthquakes in central California. a colorful rainbow. The ISLA project aims to monitor seismic- ity and study the subsurface in northwestern Louisiana over Stay tuned for more seismic updates from the field! the next 2 years. We first took delivery in Baton Rouge of a whopping 1,300 pounds of seismic equipment loaned to us by —Justin Kain, Rasheed Ajala, and Madison Menou, Louisiana the Portable Array Seismic Studies of the Continental Lith- State University; Betina Brockamp and Samantha­ Hilburn, osphere (­PASSCAL) Instrument Center and then started our Tulane University; Brennan Brunsvik, University of Louisiana installation of 10 broadband seismic stations on ­29–30 June at Lafayette; Mario Ruiz, Universidad de La Plata, Argentina; near the Texas–­ ​­Louisiana border, about a ­5-​­hour drive north Alissa Scire, IRIS PASSCAL Instrument Center; Patricia Persaud, of Baton Rouge. The photo was taken at dusk and shows us Louisiana State University; Cynthia Ebinger, Tulane University; digging a hole for one of our sensors. and Gabriele Morra, University of Louisiana at Lafayette

The deployment teams were made up mainly of a diverse group of students from Louisiana State University, Tulane University, and University of Louisiana at Lafayette. We put six stations in the ground in a record 24 hours! Our network View more postcards at bit.ly/Eos_postcard was up and running just in time to capture recordings of

48 // Eos October 2019 THE AMERICAN GEOPHYSICAL UNION IS PLEASED TO ANNOUNCE THE FOLLOWING FOR 2019:

Class of Union Fellows

Union Award, Medal, and Prize Recipients

Section Award and Lecture Honorees

For a full list of this year’s honorees please visit honors.agu.org. Registration & Housing NOW OPEN

agu.org/fallmeeting