about
Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical YearNitrogen isotopes in ice core nitrate linked to anthropogenic atmospheric acidity changeIce cores record significant 1940s Antarctic warmth related to tropical climate variabilityContinental-scale temperature variability during the past two millenniaDynamics of recent climate change in the Arctic.Strong sensitivity of Pine Island ice-shelf melting to climatic variability.Millennial-scale storminess variability in the northeastern United States during the Holocene epoch.Tropical forcing of the recent rapid Arctic warming in northeastern Canada and Greenland.Routine high-precision analysis of triple water-isotope ratios using cavity ring-down spectroscopy.The WAIS Divide deep ice core WD2014 chronology – Part 1: Methane synchronization (68–31 ka BP) and the gas age–ice age differenceSynchronous climate changes in antarctica and the north atlanticWinter warming in West Antarctica caused by central tropical Pacific warmingAntarctic temperatures over the past two centuries from ice coresInter-hemispheric temperature variability over the past millenniumA Review of Antarctic Surface Snow Isotopic Composition: Observations, Atmospheric Circulation, and Isotopic Modeling*Holocene Climate Variability in Antarctica Based on 11 Ice-Core Isotopic RecordsAn automated approach for annual layer counting in ice coresRecent climate and ice-sheet changes in West Antarctica compared with the past 2,000 yearsSeasonal climate information preserved in West Antarctic ice core water isotopes: relationships to temperature, large-scale circulation, and sea iceThe prescience of paleoclimatology and the future of the Antarctic ice sheetAn overview of air-snow exchange at Summit, Greenland: Recent experiments and findingsThe spatial extent and dynamics of the Antarctic Cold ReversalCommentary on duplicative publicationsEditorialImproved methodologies for continuous-flow analysis of stable water isotopes in ice coresAn observed negative trend in West Antarctic accumulation rates from 1975 to 2010: Evidence from new observed and simulated recordsOn the origin of the occasional spring nitrate peak in Greenland snowAssimilation of Time-Averaged Pseudoproxies for Climate ReconstructionTwentieth-century warming revives the world's northernmost lakeEvidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO 2 in the Taylor Dome, Dome C and DML ice coresGlobal atmospheric teleconnections during Dansgaard–Oeschger eventsModeled methanesulfonic acid (MSA) deposition in Antarctica and its relationship to sea iceIce Cores from the St. Elias Mountains, Yukon, Canada: Their Significance for Climate, Atmospheric Composition and Volcanism in the North Pacific RegionThe Mt Logan Holocene—late Wisconsinan isotope record: tropical Pacific—Yukon connectionsHigh-resolution ice-core stable-isotopic records from Antarctica: towards interannual climate reconstructionConstraining the recent mass balance of Pine Island and Thwaites glaciers, West Antarctica, with airborne observations of snow accumulationTropical Pacific Influence on the Source and Transport of Marine Aerosols to West Antarctica*Airborne-radar and ice-core observations of annual snow accumulation over Thwaites Glacier, West Antarctica confirm the spatiotemporal variability of global and regional atmospheric modelsIce sheet record of recent sea-ice behavior and polynya variability in the Amundsen Sea, West AntarcticaHolocene Climate Variability
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P50
description
Amerikaans glacioloog
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hulumtues
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ricercatore
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հետազոտող
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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Eric J. Steig
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Eric Julian Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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E. J. Steig
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