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The Cryosphere An interactive open-access journal of the European Geosciences Union
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We present a record of circum-Antarctic glacier and ice shelf front change over the last two decades in combination with potential environmental variables forcing retreat. Along the Antarctic coastline, glacier and ice shelf front retreat dominated between 1997–2008 and advance between 2009–2018. Decreasing sea ice days, intense snowmelt, weakening easterly winds, and relative changes in sea surface temperature were identified as enabling factors for glacier and ice shelf front retreat.
Preprints
https://doi.org/10.5194/tc-2020-224
https://doi.org/10.5194/tc-2020-224

  21 Sep 2020

21 Sep 2020

Review status: this preprint is currently under review for the journal TC.

Driving Forces of Circum-Antarctic Glacier and Ice Shelf Front Retreat over the Last Two Decades

Celia A. Baumhoer1, Andreas J. Dietz1, Christof Kneisel2, Heiko Paeth2, and Claudia Kuenzer1,2 Celia A. Baumhoer et al.
  • 1German Remote Sensing Data Center (DFD), German Aerospace Center (DLR), Muenchner Strasse 20, 82234 Wessling, Germany
  • 2Institute of Geography and Geology, University Wuerzburg, Am Hubland, 97074 Wuerzburg, Germany

Abstract. The safety band of Antarctica consisting of floating glacier tongues and ice shelves buttresses ice discharge of the Antarctic Ice Sheet. Recent disintegration events of ice shelves and glacier retreat indicate a weakening of this important safety band. Predicting calving front retreat is a real challenge due to complex ice dynamics in a data-scarce environment being unique for each ice shelf and glacier. We explore to what extent easy to access remote sensing and modelling data can help to define environmental conditions leading to calving front retreat. For the first time, we present a circum-Antarctic record of glacier and ice shelf front retreat over the last two decades in combination with environmental variables such as air temperature, sea ice days, snowmelt, sea surface temperature and wind direction. We find that the Antarctic ice sheet area shrank 29,618 ± 29 km2 in extent between 1997–2008 and gained an area of 7,108 ± 144.4 km2 between 2009 and 2018. Retreat concentrated along the Antarctic Peninsula and West Antarctica including the biggest ice shelves Ross and Ronne. Glacier and ice shelf retreat comes along with one or several changes in environmental variables. Decreasing sea ice days, intense snow melt, weakening easterlies and relative changes in sea surface temperature were identified as enabling factors for retreat. In contrast, relative increases in air temperature did not correlate with calving front retreat. To better understand drivers of glacier and ice shelf retreat it is of high importance to analyse the magnitude of basal melt through the intrusion of warm Circumpolar Deep Water (CDW) driven by strengthening westerlies and to further assess surface hydrology processes such as meltwater ponding, runoff and lake drainage.

Celia A. Baumhoer et al.

 
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Celia A. Baumhoer et al.

Celia A. Baumhoer et al.

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Latest update: 24 Jan 2021
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Short summary
We present a record of circum-Antarctic glacier and ice shelf front change over the last two decades in combination with potential environmental variables forcing retreat. Along the Antarctic coastline, glacier and ice shelf front retreat dominated between 1997–2008 and advance between 2009–2018. Decreasing sea ice days, intense snowmelt, weakening easterly winds, and relative changes in sea surface temperature were identified as enabling factors for glacier and ice shelf front retreat.
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