Adaptation and the Courtroom: Judging Climate Science
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The Contribution of Radiative Feedbacks to Orbitally Driven Climate Change
15 AUGUST 2013 E R B E T A L . 5897 The Contribution of Radiative Feedbacks to Orbitally Driven Climate Change MICHAEL P. ERB AND ANTHONY J. BROCCOLI Department of Environmental Sciences, Rutgers, The State University of New Jersey, New Brunswick, New Jersey AMY C. CLEMENT Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida (Manuscript received 2 July 2012, in final form 5 February 2013) ABSTRACT Radiative feedbacks influence Earth’s climate response to orbital forcing, amplifying some aspects of the response while damping others. To better understand this relationship, the GFDL Climate Model, version 2.1 (CM2.1), is used to perform idealized simulations in which only orbital parameters are altered while ice sheets, atmospheric composition, and other climate forcings are prescribed at preindustrial levels. These idealized simulations isolate the climate response and radiative feedbacks to changes in obliquity and longitude of the perihelion alone. Analysis shows that, despite being forced only by a redistribution of insolation with no global annual-mean component, feedbacks induce significant global-mean climate change, resulting in mean temperature changes of 20.5 K in a lowered obliquity experiment and 10.6 K in a NH winter solstice perihelion minus NH summer solstice perihelion experiment. In the obliquity ex- periment, some global-mean temperature response may be attributable to vertical variations in the transport of moist static energy anomalies, which can affect radiative feedbacks in remote regions by al- tering atmospheric stability. In the precession experiment, cloud feedbacks alter the Arctic radiation balance with possible implications for glaciation. At times when the orbital configuration favors glaciation, reductions in cloud water content and low-cloud fraction partially counteract changes in summer insolation, posing an additional challenge to understanding glacial inception. -
Thesis Paleo-Feedbacks in the Hydrological And
THESIS PALEO-FEEDBACKS IN THE HYDROLOGICAL AND ENERGY CYCLES IN THE COMMUNITY CLIMATE SYSTEM MODEL 3 Submitted by Melissa A. Burt Department of Atmospheric Science In partial fulfillment of the requirements for the Degree of Master of Science Colorado State University Fort Collins, Colorado Summer 2008 COLORADO STATE UNIVERSITY April 29, 2008 WE HEREBY RECOMMEND THAT THE THESIS PREPARED UNDER OUR SUPERVISION BY MELISSA A. BURT ENTITLED PALEO-FEEDBACKS IN THE HYDROLOGICAL AND ENERGY CYCLES IN THE COMMUNITY CLIMATE SYSTEM MODEL 3 BE ACCEPTED AS FULFILLING IN PART REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE. Committee on Graduate work ________________________________________ ________________________________________ ________________________________________ ________________________________________ ________________________________________ Adviser ________________________________________ Department Head ii ABSTRACT OF THESIS PALEO FEEDBACKS IN THE HYDROLOGICAL AND ENERGY CYCLES IN THE COMMUNITY CLIMATE SYSTEM MODEL 3 The hydrological and energy cycles are examined using the Community Climate System Model version 3 (CCSM3) for two climates, the Last Glacial Maximum (LGM) and Present Day. CCSM3, developed at the National Center for Atmospheric Research, is a coupled global climate model that simulates the atmosphere, ocean, sea ice, and land surface interactions. The Last Glacial Maximum occurred 21 ka (21,000 yrs before present) and was the cold extreme of the last glacial period with maximum extent of ice in the Northern Hemisphere. During this period, external forcings (i.e. solar variations, greenhouse gases, etc.) were significantly different in comparison to present. The “Present Day” simulation discussed in this study uses forcings appropriate for conditions before industrialization (Pre-Industrial 1750 A.D.). This research focuses on the joint variability of the hydrological and energy cycles for the atmosphere and lower boundary and climate feedbacks associated with these changes at the Last Glacial Maximum. -
Climate.2007.73.Pdf
NEWS FEATURE What’s next for the IPCC? AMANDA LEIGH HAAG Now that the Intergovernmental Panel on Climate Change has spoken more clearly than ever — and policymakers are listening — it may be time to take a new direction. Amanda Leigh Haag reports on suggested ways forward. hen the Intergovernmental Panel on Climate Change (IPCC) W was awarded the 2007 Nobel Peace Prize together with former US vice president Al Gore in October, it was a crowning moment on an already stellar year for the climate-change icon. Th e release of the IPCC’s Fourth Assessment Report (AR4) in early 2007 propelled the international body’s acronym to the status of a household name and reinforced its role as the defi nitive authority on climate change. Th e most recent report’s message was not dissimilar to those of the preceding three reports since 1990, but it came through in richer detail and with greater degrees of confi dence and consensus. Th e biggest diff erence was that this time the social climate seemed poised to receive it. “One of the reasons the Fourth Assessment was so eff ective was that the world was ready to hear it,” says Michael Oppenheimer, a climatologist PHOTOS PA at Princeton University in New Jersey and a lead author on AR4. But many are wondering what the IPCC Chairman Rajendra Pachauri, left, and United Nations Secretary-General Ban Ki-moon show the new foremost authority on climate change can synthesis report at a press conference. Scientists are now discussing what the focus and scope of future IPCC achieve from here. -
A NEW EYE on COASTS Celebrating 2 Award-Winning Years of Eos Magazine and Eos.Org
VOL. 98 NO. 1 JAN 2017 Antarctic Trek for Space Weather Partnering Academia and the Military Earth & Space Science News Whisker-like New Mineral Discovered A NEW EYE ON COASTS Celebrating 2 Award-Winning Years of Eos Magazine and Eos.org Nearly 1 Million Online Readers An International Readership Spanning 196 Countries Multiple Awards from Association TRENDS and Association Media & Publishing VOL. 97 NO. 23 1 DEC 2016 VOL. 96 NO. 4 1 MAR 2015 VOL. 96 NO. 13 15 JUL 2015 Earth & Space Science News Earth & Space Science News HowHowHow Ready ReadyReady is Isis Los Los Angeles Angeles LEARNING Sonar Data forfor thethe NextNext “ GEOSCIENCE from the Water Column “Big OneOne”? Tracking Global ? BY DOING Landslide Hazards ”? Students Launch High-Altitude Balloons Monitoring Colombia’s GEOSCIENCE Slumbering Volcanoes Seismic Hazard Assessment Lab Simulates Science Fares Well in U.S. Solar Eruptions Gender Parity Proposed Federal Budget Magnetic Islands Caterpillar-Like Motion in Space of the Greenland Ice Sheet New for 2017: You’ll receive Eos magazine once a month, and now you’ll enjoy More Content: More features, news, and Research Spotlights More Depth: Special issues on important and emerging topics The satisfaction of a reduced carbon footprint And, as always, you can read articles free online as soon as they are published on Eos.org or by adding Eos.org to mobile apps like SmartNews and Flipboard. Earth & Space Science News Contents JANUARY 2017 PROJECT UPDATE VOLUME 98, ISSUE 1 14 Space Weather from a Southern Point of View A recently completed instrument array monitors geospace from the Antarctic end of Earth’s magnetic field lines. -
Unraveling Driving Forces Explaining Significant Reduction in Satellite-Inferred Arctic Surface Albedo Since the 1980S
Unraveling driving forces explaining significant reduction in satellite-inferred Arctic surface albedo since the 1980s Rudong Zhanga,1, Hailong Wanga,1, Qiang Fub, Philip J. Rascha, and Xuanji Wangc aAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA 99352; bDepartment of Atmospheric Sciences, University of Washington, Seattle, WA 98195; and cCooperative Institute for Meteorological Satellite Studies/Space Science and Engineering Center, University of Wisconsin-Madison, Madison, WI 53706 Edited by V. Ramanathan, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, and approved October 10, 2019 (received for review September 3, 2019) The Arctic has warmed significantly since the early 1980s and sea ice cover to the observed albedo reduction. Precipitation is much of this warming can be attributed to the surface albedo projected to increase in a warmer world (20), more so in the feedback. In this study, satellite observations reveal a 1.25 to Arctic than the global mean (21, 22). This amplified increase in 1.51% per decade absolute reduction in the Arctic mean surface the Arctic has been attributed to an increase in surface evap- albedo in spring and summer during 1982 to 2014. Results from a oration associated with sea ice retreat, as well as increased global model and reanalysis data are used to unravel the causes poleward moisture transport from lower latitudes (23). Although of this albedo reduction. We find that reductions of terrestrial total precipitation is expected to increase, snowfall may de- snow cover, snow cover fraction over sea ice, and sea ice extent crease, and rainfall may dominate (24). -
For Bibliography by Year, See the Website)
THIS IS THE TEXT OF A BIBLIOGRAPHY IN THE WEB SITE “THE DISCOVERY OF GLOBAL WARMING” BY SPENCER WEART, HTTP://WWW.AIP.ORG/HISTORY/CLIMATE. FEBRUARY 2014. COPYRIGHT © 2003-2014 SPENCER WEART & AMERICAN INSTITUTE OF PHYSICS Bibliography by Author (for Bibliography by Year, see the Website) This bibliography may seem long (more than 2500 items), but it has a great many omissions. Please see the discussion of sources in the “Method” essay. Note in particular that the IPCC reports have by far the most complete bibliography for recent scientific work. Abbreviations used in the notes: AIP: Niels Bohr Library at the American Institute of Physics, College Park, MD LDEO: Lamont-Doherty Earth Observatory, Palisades, NY SIO: Scripps Institution of Oceanography Archives, La Jolla, CA Abarbenel, Albert, and Thomas McCluskey (1950). “Is the World Getting Warmer?” Saturday Evening Post, 1 July, pp. 22-23, 57-63. Abbot, Charles G., and F.E. Fowle, Jr. (1908). “Income and Outgo of Heat from the Earth, and the Dependence of Its Temperature Thereon.” Annals of the Astrophysical Observatory (Smithsonian Institution, Washington DC) 2: 159-176. Abbot, Charles G., and F.E. Fowle, Jr. (1913). “Volcanoes and Climate.” Smithsonian Miscellaneous Collections 60(29): 1-24. Abbot, Charles G. (1967). “Precipitation in Five Continents.” Smithsonian Miscellaneous Collections 151(5). Abelmann, Andrea, et al. (2006). “Extensive Phytoplankton Blooms in the Atlantic Sector of the Glacial Southern Ocean.” Paleoceanography 21: PA1013 [doi:10.1029/2005PA001199, 2006]. Abelson, P.H. (1977). “Energy and Climate.” Science 197: 941. Abe-Ouchi, Ayako, et al. (2013). “Insolation-Driven 100,000-Year Glacial Cycles and Hysteresis of Ice-Sheet Volume.” Nature 500: 190-93 [doi:10.1038/nature12374]. -
PIK-Sachbericht 2019
Inhaltsverzeichnis 01 Highlights 02 Eckdaten 03 Forschungsabteilungen 04 FutureLabs Wissenschaftsunterstützende 05 Organisationseinheiten 06 Anhang 7 United in Science 9 Von Deutschland nach Europa und in die Welt 12 Aus der Forschung 18 In eigener Sache 23 Wissenschaftliche Politikberatung 26 Medien-Highlights 2019 28 Besuche am PIK 29 Wissenschaftliche Politikberatung 30 Breitenwirkung 33 Klima, Kunst und Kultur 34 Berlin-Brandenburg – das PIK aktiv in der Heimat 36 Finanzierung | Beschäftigungszahlen 37 Publikationen | PIK in den Medien 38 Vorträge, Lehre und Veranstaltungen | Wissenschaftlicher Nachwuchs 40 Forschungsabteilung 1 – Erdsystemanalyse 46 Forschungsabteilung 2 – Klimaresilienz 52 Forschungsabteilung 3 – Transformationspfade 58 Forschungsabteilung 4 – Komplexitätsforschung 64 69 Informationstechnische Dienste 70 Verwaltung 71 Kommunikation 72 Stab der Direktoren 73 Wissenschaftsmanagement und Transfer 75 Organigramm 76 Kuratorium und Wissenschaftlicher Beirat 77 Auszeichnungen und Ernennungen 80 Berufungen, Habilitationen und Stipendien 81 Drittmittelprojekte 89 Veröff entlichungen 2019 5 Vorwort So klar man schon jetzt sagen kann, dass 2020 als Aber wir haben noch viel vor uns, das zeigt auch die das Corona-Jahr in die Geschichte eingehen wird, Pandemie-Krise, während derer dieser PIK-Sachbe- so klar lässt sich wohl auch sagen: 2019 war ein richt erstellt wurde. Die Herausforderungen werden Klima-Jahr. Klar wie nie zuvor standen Klimawandel komplexer und internationaler. Von den Planetaren und Klimapolitik im Mittelpunkt der öffentlichen Grenzen bis zu den Globalen Gemeinschaftsgütern: Aufmerksamkeit. Angestoßen durch die Fridays for Nachhaltiger Wohlstand im 21. Jahrhundert und da- Future-Bewegung gingen in Deutschland und überall rüber hinaus hängt ab vom grenzüberschreitenden auf der Welt Hunderttausende junge Menschen auf Management öff entlicher Güter – das gilt für den Ge- die Straße – unter Berufung auf die Klimaforschung, sundheitsschutz genauso wie für die Klimastabilität. -
Reducing Black Carbon May Be Fastest Strategy for Slowing Climate Change
Reducing Black Carbon May Be Fastest Strategy for Slowing Climate Change ∗ IGSD/INECE Climate Briefing Note: 29 August 2008 ∗∗ Black Carbon Is Potent Climate Forcing Agent and Key Target for Climate Mitigation Reducing black carbon (BC) may offer the greatest promise for immediate climate mitigation. BC is a potent climate forcing agent, estimated to be the second largest contributor to global warming after carbon dioxide (CO 2). Because BC remains in the atmosphere only for a few weeks, reducing BC emissions may be the fastest means of slowing climate change in the near-term. 1 Addressing BC now can help delay the possibility of passing thresholds, or tipping points, for abrupt and irreversible climate changes, 2 which could be as close as ten years away and have potentially 3 catastrophic impacts. It also can buy policymakers critical time to address CO 2 emissions in the middle and long terms. Estimates of BC’s climate forcing (combining both direct and indirect forcings) vary from the IPCC’s estimate of + 0.3 watts per square meter (W/m2) + 0.25,4 to the most recent estimate of .9 W/m 2 (see Table 1), which is “as much as 55% of the CO 2 forcing and is larger than the forcing due to the other 5 greenhouse gasses (GHGs) such as CH 4, CFCs, N 2O, or tropospheric ozone.” In some regions, such as the Himalayas, the impact of BC on melting snowpack and glaciers may be 6 equal to that of CO 2. BC emissions also significantly contribute to Arctic ice-melt, which is critical because “nothing in climate is more aptly described as a ‘tipping point’ than the 0° C boundary that separates frozen from liquid water—the bright, reflective snow and ice from the dark, heat-absorbing ocean.” 7 Hence, reducing such emissions may be “the most efficient way to mitigate Arctic warming that we know of.” 8 Since 1950, many countries have significantly reduced BC emissions, especially from fossil fuel sources, primarily to improve public health, and “technology exists for a drastic reduction of fossil fuel related BC” throughout the world. -
AMS Journals: Unsurpassed Quality, a Lasting Legacy, and Competitive Speed to Publication
LETTER FROM HEADQUARTERS AMS Journals: Unsurpassed Quality, a Lasting Legacy, and Competitive Speed to Publication hile AMS journals have always maintained a that takes the manuscript through editing, typesetting, level of quality that was unsurpassed in the and layout into final form as a high-quality archived W atmospheric and related sciences—by virtu- article in both full-function XML and PDF (plus print ally any measure you might care to focus on—there for those who still receive the journals in this format) was a period when they were less competitive is also occurring in record time—currently on the than some journals in our field when it came to the order of 60 days and improving continually. The level speed of publication. of editorial and produc- As many authors have tion work carried out happily learned in re- on manuscripts ensures cent years, this has not that the resulting article been the reality with is one that authors can AMS journals for some be proud of and one time—but the impres- that reflects well on sion still lingers in some the author when ac- quarters. So forgive cessed by scholars in me if you’ve heard this the future. before, but the steady The AMS journals improvements over re- have a long reputation cent years in the time of publishing seminal to first reviews means works, and the AMS that all the journals imprimatur is synony- making up the AMS mous with quality. AMS suite are now boasting review times in the range of authors do not need to make a choice between speed 50 days on average. -
Walter Heinrich Munk
WALTER HEINRICH MUNK 19 october 1917 . 8 february 2019 PROCEEDINGS OF THE AMERICAN PHILOSOPHICAL SOCIETY VOL. 163, NO. 3, SEPTEMBER 2019 biographical memoirs alter Heinrich Munk was a brilliant scholar and scientist who was considered one of the greatest oceanographers of W his time. He was born in Vienna, Austria in 1917 as the Austro-Hungarian Empire was declining and just before the death of one of its great artists, Gustav Klimt. Hedwig Eva Maria Kiesler, who later changed her name to Hedy Lamarr to accommodate her film career, was one of Walter’s childhood friends.1 Walter’s mother, Rega Brunner,2 the daughter of a wealthy Jewish banker, divorced Walter’s father in 1927 and married Dr. Rudolf Engelsberg in 1928. By age 14, Walter apparently had not distinguished himself in his school studies and announced that he intended to become a ski instructor. Walter later claimed that it was this that caused his mother to send him to work at a family bank in New York. The validity of this claim should be tempered by the political turmoil in Germany and its proximity to Austria. In any case, Walter left Vienna in 1932. In New York, he attended Silver Bay Preparatory School for Boys on Lake George and then became a lowly employee in the Cassel Bank, which was associated with the family’s Brunner Bank in New York. In the meantime, Walter restarted his education at Columbia’s Extension School. He greatly disliked the work at the bank and apparently made a number of mistakes, which didn’t endear him to the owners of the Cassel Bank. -
A Rational Discussion of Climate Change: the Science, the Evidence, the Response
A RATIONAL DISCUSSION OF CLIMATE CHANGE: THE SCIENCE, THE EVIDENCE, THE RESPONSE HEARING BEFORE THE SUBCOMMITTEE ON ENERGY AND ENVIRONMENT COMMITTEE ON SCIENCE AND TECHNOLOGY HOUSE OF REPRESENTATIVES ONE HUNDRED ELEVENTH CONGRESS SECOND SESSION NOVEMBER 17, 2010 Serial No. 111–114 Printed for the use of the Committee on Science and Technology ( Available via the World Wide Web: http://www.science.house.gov U.S. GOVERNMENT PRINTING OFFICE 62–618PDF WASHINGTON : 2010 For sale by the Superintendent of Documents, U.S. Government Printing Office Internet: bookstore.gpo.gov Phone: toll free (866) 512–1800; DC area (202) 512–1800 Fax: (202) 512–2104 Mail: Stop IDCC, Washington, DC 20402–0001 COMMITTEE ON SCIENCE AND TECHNOLOGY HON. BART GORDON, Tennessee, Chair JERRY F. COSTELLO, Illinois RALPH M. HALL, Texas EDDIE BERNICE JOHNSON, Texas F. JAMES SENSENBRENNER JR., LYNN C. WOOLSEY, California Wisconsin DAVID WU, Oregon LAMAR S. SMITH, Texas BRIAN BAIRD, Washington DANA ROHRABACHER, California BRAD MILLER, North Carolina ROSCOE G. BARTLETT, Maryland DANIEL LIPINSKI, Illinois VERNON J. EHLERS, Michigan GABRIELLE GIFFORDS, Arizona FRANK D. LUCAS, Oklahoma DONNA F. EDWARDS, Maryland JUDY BIGGERT, Illinois MARCIA L. FUDGE, Ohio W. TODD AKIN, Missouri BEN R. LUJA´ N, New Mexico RANDY NEUGEBAUER, Texas PAUL D. TONKO, New York BOB INGLIS, South Carolina STEVEN R. ROTHMAN, New Jersey MICHAEL T. MCCAUL, Texas JIM MATHESON, Utah MARIO DIAZ-BALART, Florida LINCOLN DAVIS, Tennessee BRIAN P. BILBRAY, California BEN CHANDLER, Kentucky ADRIAN SMITH, Nebraska RUSS CARNAHAN, Missouri PAUL C. BROUN, Georgia BARON P. HILL, Indiana PETE OLSON, Texas HARRY E. MITCHELL, Arizona CHARLES A. WILSON, Ohio KATHLEEN DAHLKEMPER, Pennsylvania ALAN GRAYSON, Florida SUZANNE M. -
Cloud Feedback Mechanisms and Their Representation in Global Climate Models Paulo Ceppi ,1* Florent Brient ,2 Mark D
Advanced Review Cloud feedback mechanisms and their representation in global climate models Paulo Ceppi ,1* Florent Brient ,2 Mark D. Zelinka 3 and Dennis L. Hartmann 4 Edited by Eduardo Zorita, Domain Editor and Editor-in-Chief Cloud feedback—the change in top-of-atmosphere radiative flux resulting from the cloud response to warming—constitutes by far the largest source of uncer- tainty in the climate response to CO2 forcing simulated by global climate models (GCMs). We review the main mechanisms for cloud feedbacks, and discuss their representation in climate models and the sources of intermodel spread. Global- mean cloud feedback in GCMs results from three main effects: (1) rising free- tropospheric clouds (a positive longwave effect); (2) decreasing tropical low cloud amount (a positive shortwave [SW] effect); (3) increasing high-latitude low cloud optical depth (a negative SW effect). These cloud responses simulated by GCMs are qualitatively supported by theory, high-resolution modeling, and observa- tions. Rising high clouds are consistent with the fixed anvil temperature (FAT) hypothesis, whereby enhanced upper-tropospheric radiative cooling causes anvil cloud tops to remain at a nearly fixed temperature as the atmosphere warms. Tropical low cloud amount decreases are driven by a delicate balance between the effects of vertical turbulent fluxes, radiative cooling, large-scale subsidence, and lower-tropospheric stability on the boundary-layer moisture budget. High- latitude low cloud optical depth increases are dominated by phase changes in mixed-phase clouds. The causes of intermodel spread in cloud feedback are dis- cussed, focusing particularly on the role of unresolved parameterized processes such as cloud microphysics, turbulence, and convection.