Synchronous Volcanic Eruptions and Abrupt Climate Change ∼17.7 Ka Plausibly Linked by Stratospheric Ozone Depletion
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Lecture 21: Glaciers and Paleoclimate Read: Chapter 15 Homework Due Thursday Nov
Learning Objectives (LO) Lecture 21: Glaciers and Paleoclimate Read: Chapter 15 Homework due Thursday Nov. 12 What we’ll learn today:! 1. 1. Glaciers and where they occur! 2. 2. Compare depositional and erosional features of glaciers! 3. 3. Earth-Sun orbital parameters, relevance to interglacial periods ! A glacier is a river of ice. Glaciers can range in size from: 100s of m (mountain glaciers) to 100s of km (continental ice sheets) Most glaciers are 1000s to 100,000s of years old! The Snowline is the lowest elevation of a perennial (2 yrs) snow field. Glaciers can only form above the snowline, where snow does not completely melt in the summer. Requirements: Cold temperatures Polar latitudes or high elevations Sufficient snow Flat area for snow to accumulate Permafrost is permanently frozen soil beneath a seasonal active layer that supports plant life Glaciers are made of compressed, recrystallized snow. Snow buildup in the zone of accumulation flows downhill into the zone of wastage. Glacier-Covered Areas Glacier Coverage (km2) No glaciers in Australia! 160,000 glaciers total 47 countries have glaciers 94% of Earth’s ice is in Greenland and Antarctica Mountain Glaciers are Retreating Worldwide The Antarctic Ice Sheet The Greenland Ice Sheet Glaciers flow downhill through ductile (plastic) deformation & by basal sliding. Brittle deformation near the surface makes cracks, or crevasses. Antarctic ice sheet: ductile flow extends into the ocean to form an ice shelf. Wilkins Ice shelf Breakup http://www.youtube.com/watch?v=XUltAHerfpk The Greenland Ice Sheet has fewer and smaller ice shelves. Erosional Features Unique erosional landforms remain after glaciers melt. -
Minimal Geological Methane Emissions During the Younger Dryas-Preboreal Abrupt Warming Event
UC San Diego UC San Diego Previously Published Works Title Minimal geological methane emissions during the Younger Dryas-Preboreal abrupt warming event. Permalink https://escholarship.org/uc/item/1j0249ms Journal Nature, 548(7668) ISSN 0028-0836 Authors Petrenko, Vasilii V Smith, Andrew M Schaefer, Hinrich et al. Publication Date 2017-08-01 DOI 10.1038/nature23316 Peer reviewed eScholarship.org Powered by the California Digital Library University of California LETTER doi:10.1038/nature23316 Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event Vasilii V. Petrenko1, Andrew M. Smith2, Hinrich Schaefer3, Katja Riedel3, Edward Brook4, Daniel Baggenstos5,6, Christina Harth5, Quan Hua2, Christo Buizert4, Adrian Schilt4, Xavier Fain7, Logan Mitchell4,8, Thomas Bauska4,9, Anais Orsi5,10, Ray F. Weiss5 & Jeffrey P. Severinghaus5 Methane (CH4) is a powerful greenhouse gas and plays a key part atmosphere can only produce combined estimates of natural geological in global atmospheric chemistry. Natural geological emissions and anthropogenic fossil CH4 emissions (refs 2, 12). (fossil methane vented naturally from marine and terrestrial Polar ice contains samples of the preindustrial atmosphere and seeps and mud volcanoes) are thought to contribute around offers the opportunity to quantify geological CH4 in the absence of 52 teragrams of methane per year to the global methane source, anthropogenic fossil CH4. A recent study used a combination of revised 13 13 about 10 per cent of the total, but both bottom-up methods source δ C isotopic signatures and published ice core δ CH4 data to 1 −1 2 (measuring emissions) and top-down approaches (measuring estimate natural geological CH4 at 51 ± 20 Tg CH4 yr (1σ range) , atmospheric mole fractions and isotopes)2 for constraining these in agreement with the bottom-up assessment of ref. -
Integrated Tephrochonology Copyedited
U.S. Geological Survey and The National Academies; USGS OFR-2007-xxxx, Extended Abstract.yyy, 1- Integrated tephrochronology of the West Antarctic region- Implications for a potential tephra record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core N.W. Dunbar,1 W.C. McIntosh,1 A.V. Kurbatov,2 and T.I Wilch 3 1NMGB/EES Department, New Mexico Tech, Socorro NM, 87801, USA ( [email protected] , [email protected] ) 2Climate Change Institute 303 Bryand Global Sciences Center, Orono, ME, 04469, USA ([email protected]) 3Department of Geological Sciences, Albion College, Albion MI, 49224, USA ( [email protected] ) Summary Mount Berlin and Mt. Takahe, two West Antarctica volcanic centers have produced a number of explosive, ashfall generating eruptions over the past 500,000 yrs. These eruptions dispersed volcanic ash over large areas of the West Antarctic ice sheet. Evidence of these eruptions is observed at two blue ice sites (Mt. Waesche and Mt. Moulton) as well as in the Siple Dome and Byrd (Palais et al., 1988) ice cores. Geochemical correlations between tephra sampled at the source volcanoes, at blue ice sites, and in the Siple Dome ice core suggest that at least some of the eruptions covered large areas of the ice sheet with a volcanic ash, and 40 Ar/ 39 Ar dating of volcanic material provides precise timing when these events occurred. Volcanic ash from some of these events expected to be found in the WAIS Divide ice core, providing chronology and inter-site correlation. Citation: Dunbar, N.W., McIntosh, W.C., Kurbatov, A., and T.I Wilch (2007), Integrated tephrochronology of the West Antarctic region- Implications for a potential tephra record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10 th ISAES X, edited by A. -
Tephrochronology: Methodology and Correlations, Antarctic Peninsula Area
Tephrochronology: Methodology and correlations, Antarctic Peninsula Area Mats Molén Thesis in Physical Geography 30 ECTS Master’s Level Report passed: November 9 2012 Supervisor: Rolf Zale Tephrochronology: Methodology and correlations, Antarctic Peninsula Area Abstract Methods for tephrochronology are evaluated, in the following way: Lake sediments <500 years old from three small Antarctic lakes were analysed for identification of tephras. Subsamples were analysed for a) grain size, and identification and concentration of volcanogenic grains, b) identification of tephra horizons, c) element abundance by EPMA WDS/EDS and LA-ICP-MS, and d) possible correlations between lakes and volcanoes. Volcanogenic minerals and shards were found all through the sediment cores in all three lakes, in different abundances. A high background population of volcanogenic mineral grains, in all samples, made the identification of tephra horizons difficult, and shards could only be distinguished by certainty after chemical analysis of elements. The tephra layers commonly could not be seen by the naked eye, and, hence they are regarded as cryptotephras. Because of the small size of recent eruptions in the research area, and the travel distance of ash, most shards are small and difficult to analyse. Nine possible tephra horizons have been recorded in the three lakes, and preliminary correlations have been made. But because of analytical problems, the proposed correlations between the lakes and possible volcanic sources are preliminary. Table of contents 1. Introduction . 1 1.1. Advances and problems of tephrochronology . 1 1.1.1. General observations .. 1 1.1.2. Difficulties in tephrochronology work .. 2 1.1.3. The current research .. 4 1.2. -
Sea Level and Climate Introduction
Sea Level and Climate Introduction Global sea level and the Earth’s climate are closely linked. The Earth’s climate has warmed about 1°C (1.8°F) during the last 100 years. As the climate has warmed following the end of a recent cold period known as the “Little Ice Age” in the 19th century, sea level has been rising about 1 to 2 millimeters per year due to the reduction in volume of ice caps, ice fields, and mountain glaciers in addition to the thermal expansion of ocean water. If present trends continue, including an increase in global temperatures caused by increased greenhouse-gas emissions, many of the world’s mountain glaciers will disap- pear. For example, at the current rate of melting, most glaciers will be gone from Glacier National Park, Montana, by the middle of the next century (fig. 1). In Iceland, about 11 percent of the island is covered by glaciers (mostly ice caps). If warm- ing continues, Iceland’s glaciers will decrease by 40 percent by 2100 and virtually disappear by 2200. Most of the current global land ice mass is located in the Antarctic and Greenland ice sheets (table 1). Complete melt- ing of these ice sheets could lead to a sea-level rise of about 80 meters, whereas melting of all other glaciers could lead to a Figure 1. Grinnell Glacier in Glacier National Park, Montana; sea-level rise of only one-half meter. photograph by Carl H. Key, USGS, in 1981. The glacier has been retreating rapidly since the early 1900’s. -
Calving Processes and the Dynamics of Calving Glaciers ⁎ Douglas I
Earth-Science Reviews 82 (2007) 143–179 www.elsevier.com/locate/earscirev Calving processes and the dynamics of calving glaciers ⁎ Douglas I. Benn a,b, , Charles R. Warren a, Ruth H. Mottram a a School of Geography and Geosciences, University of St Andrews, KY16 9AL, UK b The University Centre in Svalbard, PO Box 156, N-9171 Longyearbyen, Norway Received 26 October 2006; accepted 13 February 2007 Available online 27 February 2007 Abstract Calving of icebergs is an important component of mass loss from the polar ice sheets and glaciers in many parts of the world. Calving rates can increase dramatically in response to increases in velocity and/or retreat of the glacier margin, with important implications for sea level change. Despite their importance, calving and related dynamic processes are poorly represented in the current generation of ice sheet models. This is largely because understanding the ‘calving problem’ involves several other long-standing problems in glaciology, combined with the difficulties and dangers of field data collection. In this paper, we systematically review different aspects of the calving problem, and outline a new framework for representing calving processes in ice sheet models. We define a hierarchy of calving processes, to distinguish those that exert a fundamental control on the position of the ice margin from more localised processes responsible for individual calving events. The first-order control on calving is the strain rate arising from spatial variations in velocity (particularly sliding speed), which determines the location and depth of surface crevasses. Superimposed on this first-order process are second-order processes that can further erode the ice margin. -
Multiple Sources for Tephra from AD 1259 Volcanic Signal in Antarctic Ice
Multiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino To cite this version: Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino. Mul- tiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores. Quaternary Science Reviews, Elsevier, 2019, 210, pp.164-174. 10.1016/j.quascirev.2019.03.005. hal-02350371 HAL Id: hal-02350371 https://hal.archives-ouvertes.fr/hal-02350371 Submitted on 25 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Manuscript Details Manuscript number JQSR_2019_21 Title MULTIPLE SOURCES FOR TEPHRA FROM AD 1259 VOLCANIC SIGNAL IN ANTARCTIC ICE CORES Abstract Strong volcanic signals simultaneously recorded in polar ice sheets are commonly assigned to major low-latitude eruptions that dispersed large quantities of aerosols in the global atmosphere with the potential of inducing climate perturbations. Parent eruptions responsible for specific events are typically deduced from matching to a known volcanic eruption having coincidental date. However, more robust source linkage can be achieved only through geochemical characterisation of the airborne volcanic glass products (tephra) sometimes preserved in the polar strata. -
Igneous Rocks of Peter I Island Hemisphere Tectonic Reconstructions
LeMasurier, W. E., and F. A. Wade. In press. Volcanic history in Marie Byrd Land: implications with regard to southern Igneous rocks of Peter I Island hemisphere tectonic reconstructions. In: Proceedings of the International Symposium on Andean and Antarctic Vol- canology Problems, Santiago, Chile (0. Gonzalez-Ferran, edi- tor). Rome, International Association of Volcanology and Chemistry of Earths Interior. THOMAS W. BASTIEN Price, R. C., and S. R. Taylor. 1973. The geochemistry of Dune- Ernest E. Lehmann Associates din Volcano, East Otago, New Zealand: rare earth elements. Minneapolis, Minnesota 55403 Contributions to Mineralogy and Petrology, 40: 195-205. Sun, S. S., and G. N. Hanson. 1975. Origin of Ross Island basanitoids and limitations upon the heterogeneity of mantle CAMPBELL CRADDOCK sources of alkali basalts and nephelinites. Contributions to Department of Geology and Geophysics Mineralogy and Petrology, 52: 77-106. The University of Wisconsin, Madison Sun, S. S., and G. N. Hanson. 1976. Rare earth element evi- Madison, Wisconsin 53706 dence for differentiation of McMurdo volcanics, Ross Island, Antarctica. Contributions to Mineralogy and Petrology, 54: 139-155. Peter I Island lies in the southeastern Pacific Ocean at 68°50S. 90°40W. about 240 nautical miles off the Eights Coast of West Antarctica. Ris- ing from the continental rise, it is one of the few truly oceanic islands in the region. Few people have been on the island, and little is known of its geology. Thaddeus von Bellingshausen discovered and named the island in 1821, and it was not seen again until sighted by Pierre Charcot in 1910. A Nor- wegian ship dredged some rocks off the west coast in 1927, and persons from the Norvegia achieved the first landing in 1929. -
Abrupt Climate Change in the Computer: Is It Real?
Perspective Abrupt climate change in the computer: Is it real? Thomas F. Stocker* and Olivier Marchal Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland Models suggest that dramatic changes in the ocean circulation are responsible for abrupt climate changes during the last ice age and may possibly alter the relative climate stability of the last 10,000 years. mong the archives recording past cli- the air–sea fluxes of heat and freshwater. In freshwater balance of the North Atlantic. By Amate and environmental changes, ice the Pacific there is no such circulation, be- discharging freshwater, the thermohaline cores, marine and lacustrine sediments in cause the surface waters are too fresh: even circulation reduces or collapses completely, anoxic environments, and tree rings have if cooled to the freezing point, they would but the response depends on the location, seasonal to annual resolution. Changes in not acquire enough density to sink down and amplitude and duration of the perturbation dust level (1), snow accumulation (2), sum- establish a large-scale THC. This is caused (11, 12, 14, 15, 17, 18). All three responses mer temperature (3), and indicators of the by a combination of several factors, includ- shown in Fig. 1 can be generated in such productivity of marine life (4) suggest that ing reduced evaporation in the Pacific, models, albeit at different threshold values. some of the climate changes have evolved on fresher surface waters flowing northward, The Younger Dryas cold event (12,700– time scales as short as a few years to decades. -
What If Antarctica's Volcanoes Erupt
What if Antarctica's dormant, ice-covered volcanoes wake up? John Smellie, Department of Geology, University of Leicester (This article was originally published in The Conversation, on 4 September 2017 [https://theconversation.com/what-if-antarcticas-dormant-ice-covered-volcanoes-wake-up-83450]) Antarctica is a vast icy wasteland covered by the world’s largest ice sheet. This ice sheet contains about 90% of fresh water on the planet. It acts as a massive heat sink and its meltwater drives the world’s oceanic circulation. Its existence is therefore a fundamental part of Earth’s climate. Less well known is that Antarctica is also host to several active volcanoes, part of a huge "volcanic province" which extends for thousands of kilometres along the Western edge of the continent. Although the volcanic province has been known and studied for decades, recently about 100 "new" volcanoes were recently discovered beneath the ice by scientists who used satellite data and ice- penetrating radar to search for hidden peaks. These sub-ice volcanoes may be dormant. But what would happen if Antarctica’s volcanoes awoke? IMAGE: Some of the volcanoes known about before the latest discovery. Source: antarcticglaciers.org (image: JL Smellie) We can get some idea by looking to the past. One of Antarctica’s volcanoes, Mount Takahe, is found close to the remote centre of the West Antarctic Ice Sheet. In a new study, scientists implicate Takahe in a series of eruptions rich in ozone-consuming halogens that occurred about 18,000 years ago. These eruptions, they claim, triggered an ancient ozone hole, warmed the southern hemisphere causing glaciers to melt, and helped bring the last ice age to a close. -
An Abrupt Climate Change Scenario and Its Implications for United States National Security October 2003
An Abrupt Climate Change Scenario and Its Implications for United States National Security October 2003 By Peter Schwartz and Doug Randall Imagining the Unthinkable The purpose of this report is to imagine the unthinkable – to push the boundaries of current research on climate change so we may better understand the potential implications on United States national security. We have interviewed leading climate change scientists, conducted additional research, and reviewed several iterations of the scenario with these experts. The scientists support this project, but caution that the scenario depicted is extreme in two fundamental ways. First, they suggest the occurrences we outline would most likely happen in a few regions, rather than on globally. Second, they say the magnitude of the event may be considerably smaller. We have created a climate change scenario that although not the most likely, is plausible, and would challenge United States national security in ways that should be considered immediately. Executive Summary There is substantial evidence to indicate that significant global warming will occur during the 21st century. Because changes have been gradual so far, and are projected to be similarly gradual in the future, the effects of global warming have the potential to be manageable for most nations. Recent research, however, suggests that there is a possibility that this gradual global warming could lead to a relatively abrupt slowing of the ocean’s thermohaline conveyor, which could lead to harsher winter weather conditions, sharply reduced soil moisture, and more intense winds in certain regions that currently provide a significant fraction of the world’s food production. -
This Document Has Been Archived
This document has been archived. U.S. Antarctic Program, 1998-1999 ......................... iii Biology and medical research .................................. 1 Long-term ecological research.................................14 Environmental research..........................................16 Geology and geophysics ..........................................17 Glaciology .............................................................35 Ocean and climate studies ......................................40 Aeronomy and astrophysics ....................................45 Technical projects..................................................56 U.S. Antarctic Program, 1998-1999 iii U.S. Antarctic Program, 1998-1999 In Antarctica, the U.S. Antarctic Program will · a U.S.–French–Australian collaboration to support 142 research projects during the 1998- study katabatic winds along the coast of 1999 austral summer and the 1999 austral East Antarctica winter at the three U.S. stations (McMurdo, · continued support of the Center for Astro- Amundsen-Scott South Pole, and Palmer), physical Research in Antarctica at the geo- aboard its two research ships (Laurence M. graphic South Pole Gould and Nathaniel B. Palmer) in the Ross Sea and in the Antarctic Peninsula region, at re- · measuring, monitoring, and studying at- mote field camps, and in cooperation with the mospheric trace gases associated with the national antarctic programs of the other Ant- annual depletion of the ozone layer above arctic Treaty nations. Many of the projects Antarctica. that make up the program, which is funded Science teams will also make use of a conti- and managed by the National Science Foun- nent-wide network of automatic weather sta- dation (NSF), are part of the international ef- tions, a network of six automated geophysical fort to understand the Antarctic and its role in observatories, ultraviolet-radiation monitors global processes. NSF also supports research at the three U.S.