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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Ice sheets--Congresses. ; Electronic books.
    Description / Table of Contents: Proceedings of the NATO Advanced Research Workshop Ice in the Climate System, held at Aussois, France, September 6-12, 1992.
    Type of Medium: Online Resource
    Pages: 1 online resource (670 pages)
    Edition: 1st ed.
    ISBN: 9783642850165
    Series Statement: Nato asi Subseries I: Series ; v.12
    DDC: 551.52
    Language: English
    Note: Intro -- Ice in the Climate System -- Copyright -- TABLE OF CONTENTS -- PROLOGUE -- LIST OF AUTHORS AND PARTICIPANTS -- EXTENT AND MELTING HISTORY OF THE LATE WEICHSELIAN ICE SHEET, THE BARENTS-KARA CONTINENTAL MARGIN -- MODELLING OF THE FENNOSCANDIAN ICE SHEET -- CONTROLS ON CHANGES IN THE WEST ANTARCTIC ICE SHEET -- PLASTIC MODELLING OF GLACIERS AND OUTLETS -- QUALITATIVE DYNAMICS OF MARINE ICE SHEETS -- MODELLING OF GLACIER MASS BALANCE -- OBSERVATIONS AND SIMULATIONS OF TEMPERATURE AND ICE ACCUMULATION AT THE SURFACE OF ANTARCTICA -- WORLD SEA LEVEL AND THE PRESENT MASS BALANCE OF THE ANTARCTIC ICE SHEET -- ICE, CLIMATE, AND SEA LEVEL -- DO WE KNOW WHAT IS HAPPENING? -- HEINRICH EVENTS: TRIGGERS OF OCEAN CIRCULATION CHANGE? -- HEINRICH EVENTS: CHRONOLOGY AND PROCESSES, EAST-CENTRAL LAURENTIDE ICE SHEET AND NW LABRADOR SEA -- Transport of Freshwater into the Deep Ocean by the Conveyor -- The driving force of brine rejection on the deepwater formation in the Hamburg LSG OGCM. -- THE MELTING OF CONTINENTAL ICE IN THE OCEAN AND ITS IMPACT ON SURFACE AND BOTTOM WATERS -- HYDROLOGICAL CYCLE SCENARIOS, DEEP OCEAN CIRCULATION, AND CENTURY/MILLENNIUM CLIMATE CHANGE: A SIMULATION STUDY USING AN OCEAN-ATMOSPHERE-ICE SHEET MODEL -- A SIMPLE SYSTEMS MODEL OF THE MAJOR GLACIATION CYCLES -- CLIMATE MODEL STUDIES OF INTERACTIONS BETWEEN ICE SHEETS AND THE ATMOSPHERE-OCEAN SYSTEM -- MODELLING ICE SHEET AND CLIMATE CHANGES THROUGH THE ICE AGES -- SIMULATION OF THE CLIMATE OF THE LAST 200 KYR WITH THE LLN 2D-MODEL -- THE LATE CENOZOIC GLACIAL REGIMES AS A COMBINED RESPONSE TO EARTH-ORBITAL VARIATIONS AND FORCED AND FREE CO2 VARIATIONS -- THE DELICACY OF THE OCEANIC THERMOHALINE CIRCULATION -- Multiple equilibria in β-plane thermohaline convection -- YOUNGER DRYAS EXPERIMENTS -- DEEP DECOUPLING OSCILLATIONS OF THE OCEANIC THERMOHALINE CIRCULATION. , THE GLACIAL OCEAN: A STUDY WITH A ZONALLY AVERAGED, THREE-BASIN OCEAN CIRCULATION MODEL -- OSCILLATORY MODES OF BEHAVIOR IN A SIMPLE MODEL OF THE ATLANTIC THERMOHALINE CIRCULATION -- CORRELATION OF GREENLAND ICE-CORE AND ICE-MARGIN δ(18O) RECORDS -- THE CONNECTION BETWEEN ICE DYNAMICS AND PALEOCLIMATE FROM ICE CORES: A STUDY OF TAYLOR DOME, ANTARCTICA -- Past Accumulation rates derived from observed annual layers in the GRIP ice core from Summit, Central Greenland. -- SEA ICE: A FACTOR IN INFLUENCING CLIMATE ON SHORT AND LON TIME SCALES -- NONLINEAR PALEOCLIMATIC VARIABILITY FROM QUATERNARY RECORDS -- THE ARCTIC RESPONSE TO CO2-INDUCED WARMING IN A COUPLED ATMOSPHERE-OCEAN GENERAL CIRCULATION MODEL -- OCEAN HEAT AND SEASONAL SEA ICE THICKNESS IN THE SOUTHERN OCEAN -- QUANTITATIVE RECONSTRUCTION OF SEA-SURFACE CONDITIONS, SEASONAL EXTENT OF SEA-ICE COVER AND MELTWATER DISCHARGES IN HIGH LATITUDE MARINE ENVIRONMENTS FROM DINOFLAGELLATE CYST ASSEMBLAGES -- NORTH ATLANTIC SEA SURFACE SALINITY, ICE MELTING AND ABRUPT CLIMATIC CHANGES -- INTERANNUAL AND CLIMATIC CHARACTERISTICS OF AN ICE OCEAN CIRCULATION MODEL -- A THERMODYNAMIC-DYNAMIC SNOW SEA-ICE MODEL.
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  • 2
    Publication Date: 2019-01-25
    Description: Analysis | Published: 13 June 2018 Mass balance of the Antarctic Ice Sheet from 1992 to 2017 The IMBIE team Naturevolume 558, pages219–222 (2018) | Download Citation Abstract The Antarctic Ice Sheet is an important indicator of climate change and driver of sea-level rise. Here we combine satellite observations of its changing volume, flow and gravitational attraction with modelling of its surface mass balance to show that it lost 2,720 ± 1,390 billion tonnes of ice between 1992 and 2017, which corresponds to an increase in mean sea level of 7.6 ± 3.9 millimetres (errors are one standard deviation). Over this period, ocean-driven melting has caused rates of ice loss from West Antarctica to increase from 53 ± 29 billion to 159 ± 26 billion tonnes per year; ice-shelf collapse has increased the rate of ice loss from the Antarctic Peninsula from 7 ± 13 billion to 33 ± 16 billion tonnes per year. We find large variations in and among model estimates of surface mass balance and glacial isostatic adjustment for East Antarctica, with its average rate of mass gain over the period 1992–2017 (5 ± 46 billion tonnes per year) being the least certain.
    Description: Published
    Description: 219-222
    Description: 5A. Paleoclima e ricerche polari
    Description: JCR Journal
    Keywords: Antarctica ; Ice sheet mass balance ; 02.02. Glaciers ; 04.03. Geodesy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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