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  • -; DATE/TIME; East Greenland; Error, absolute; Event label; Glacier; Glacier discharge; Glacier mass, flux; Glacier width; Helheim_glacier; International Polar Year (2007-2008); IPY; Jakobshavn_Isbrae; Kangerdlugssuaq_gl; MULT; Multiple investigations; Sermilik Fjord, SE Greenland; West Greenland  (1)
  • 02.02. Glaciers  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Howat, Ian M; Ahn, Yushin; Joughin, Ian; van den Broeke, Michiel R; Lenaerts, Jan T M; Smith, Ben E (2011): Mass balance of Greenland's three largest outlet glaciers, 2000-2010. Geophysical Research Letters, 38(12), L12501, https://doi.org/10.1029/2011GL047565
    Publication Date: 2023-12-13
    Description: Acceleration of Greenland's three largest outlet glaciers, Helheim, Kangerdlugssuaq and Jakobshavn Isbræ, accounted for a substantial portion of the ice sheet's mass loss over the past decade. Rapid changes in their discharge, however, make their cumulative mass-change uncertain. We derive monthly mass balance rates and cumulative balance from discharge and surface mass balance (SMB) rates for these glaciers from 2000 through 2010. Despite the dramatic changes observed at Helheim, the glacier gained mass over the period, due primarily to the short duration of acceleration and a likely longer-term positive balance. In contrast, Jakobshavn Isbræ lost an equivalent of over 11 times the average annual SMB and loss continues to accelerate. Kangerdlugssuaq lost over 7 times its annual average SMB, but loss has returned to the 2000 rate. These differences point to contrasts in the long-term evolution of these glaciers and the danger in basing predictions on extrapolations of recent changes.
    Keywords: -; DATE/TIME; East Greenland; Error, absolute; Event label; Glacier; Glacier discharge; Glacier mass, flux; Glacier width; Helheim_glacier; International Polar Year (2007-2008); IPY; Jakobshavn_Isbrae; Kangerdlugssuaq_gl; MULT; Multiple investigations; Sermilik Fjord, SE Greenland; West Greenland
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
    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
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