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  • Antarctica; DF; Dome_Fuji; Dome C; Dome C, Antarctica; DRILL; Drilling/drill rig; EDC; EDML; EDRILL; Electromechanical drill; EMD; EPICA-Campaigns; EPICA Dome C; EPICA drill; EPICA Dronning Maud Land, DML28C01_00; ICEDRILL; Ice drill; Kohnen Station; Sampling/drilling ice; TALDICE; Talos Dome; Taylor_Dome; TAYLOR_DOME; TD; THERM; Thermal drill; VK; VOSTOK; VOSTOK_Hole#3G-2  (1)
  • Ice sheet mass balance  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Masson-Delmotte, Valerie; Buiron, Daphné; Ekaykin, Alexey A; Frezzotti, Massimo; Gallée, Hubert; Jouzel, Jean; Krinner, Gerhard; Landais, Amaëlle; Motoyama, Hideaki; Oerter, Hans; Pol, Katy; Pollard, David; Ritz, Catherine; Schlosser, Elisabeth; Sime, Louise C; Sodemann, Harald; Stenni, Barbara; Uemura, Ryu; Vimeux, Françoise (2011): A comparison of the present and last interglacial periods in six Antarctic ice cores. Climate of the Past, 7, 397-423, https://doi.org/10.5194/cp-7-397-2011
    Publication Date: 2023-07-19
    Description: We compare the present and last interglacial periods as recorded in Antarctic water stable isotope records now available at various temporal resolutions from six East Antarctic ice cores: Vostok, Taylor Dome, EPICA Dome C (EDC), EPICA Dronning Maud Land (EDML), Dome Fuji and the recent TALDICE ice core from Talos Dome. We first review the different modern site characteristics in terms of ice flow, meteorological conditions, precipitation intermittency and moisture origin, as depicted by meteorological data, atmospheric reanalyses and Lagrangian moisture source diagnostics. These different factors can indeed alter the relationships between temperature and water stable isotopes. Using five records with sufficient resolution on the EDC3 age scale, common features are quantified through principal component analyses. Consistent with instrumental records and atmospheric model results, the ice core data depict rather coherent and homogenous patterns in East Antarctica during the last two interglacials. Across the East Antarctic plateau, regional differences, with respect to the common East Antarctic signal, appear to have similar patterns during the current and last interglacials. We identify two abrupt shifts in isotopic records during the glacial inception at TALDICE and EDML, likely caused by regional sea ice expansion. These regional differences are discussed in terms of moisture origin and in terms of past changes in local elevation histories, which are compared to ice sheet model results. Our results suggest that elevation changes may contribute significantly to inter-site differences. These elevation changes may be underestimated by current ice sheet models
    Keywords: Antarctica; DF; Dome_Fuji; Dome C; Dome C, Antarctica; DRILL; Drilling/drill rig; EDC; EDML; EDRILL; Electromechanical drill; EMD; EPICA-Campaigns; EPICA Dome C; EPICA drill; EPICA Dronning Maud Land, DML28C01_00; ICEDRILL; Ice drill; Kohnen Station; Sampling/drilling ice; TALDICE; Talos Dome; Taylor_Dome; TAYLOR_DOME; TD; THERM; Thermal drill; VK; VOSTOK; VOSTOK_Hole#3G-2
    Type: Dataset
    Format: application/zip, 13 datasets
    Location Call Number Limitation Availability
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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
    Location Call Number Limitation Availability
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