Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ...
Mass changes of polar ice sheets have an important societal impact, because they affect global sea level. Estimating the current mass budget of ice sheets is equivalent to determining the balance between surface mass gain through precipitation and outflow across the grounding line. For the Antarctic...
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ftdatacite:10.1594/pangaea.836299 2024-09-15T17:41:06+00:00 Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ... Callens, Denis Matsuoka, Kenichi Steinhage, Daniel Pattyn, Frank 2015 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.836299 https://doi.pangaea.de/10.1594/PANGAEA.836299 en eng PANGAEA https://dx.doi.org/10.3189/2015aog70a010 https://dx.doi.org/10.5194/tc-8-867-2014 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 LATITUDE LONGITUDE Surface elevation Ice thickness, glacier Multiple investigations Airborne radio-echo sounding dataset Supplementary Dataset Dataset 2015 ftdatacite https://doi.org/10.1594/pangaea.83629910.3189/2015aog70a01010.5194/tc-8-867-2014 2024-08-01T10:52:43Z Mass changes of polar ice sheets have an important societal impact, because they affect global sea level. Estimating the current mass budget of ice sheets is equivalent to determining the balance between surface mass gain through precipitation and outflow across the grounding line. For the Antarctic ice sheet, grounding line outflow is governed by oceanic processes and outlet glacier dynamics. In this study, we compute the mass budget of major outlet glaciers in the eastern Dronning Maud Land sector of the Antarctic ice sheet using the input/output method. Input is given by recent surface accumulation estimates (SMB) of the whole drainage basin. The outflow at the grounding line is determined from the radar data of a recent airborne survey and satellite-based velocities using a flow model of combined plug flow and simple shear. This approach is an improvement on previous studies, as the ice thickness is measured, rather than being estimated from hydrostatic equilibrium. In line with the general thickening of ... : Geographic coordinates were collected with GPS. Surface elevation is the elevation of the plane (from GPS) corrected for the distance between the plane and the surface measured with laser altimeter. Ice thickness is reconstructed by picking the bed wave on radargram collected with 150-Mhz AWI's airborne radar. The two-way travel time is converted into thickness assuming a constant propagation speed of 168E+006 m/s.These data were collected with the financial support of EUropean Facility for Airborne Research (EUFAR, http://www.eufar.net). ... Dataset Antarc* Antarctic Antarctica Dronning Maud Land Ice Sheet DataCite |
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Open Polar |
collection |
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ftdatacite |
language |
English |
topic |
LATITUDE LONGITUDE Surface elevation Ice thickness, glacier Multiple investigations Airborne radio-echo sounding |
spellingShingle |
LATITUDE LONGITUDE Surface elevation Ice thickness, glacier Multiple investigations Airborne radio-echo sounding Callens, Denis Matsuoka, Kenichi Steinhage, Daniel Pattyn, Frank Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ... |
topic_facet |
LATITUDE LONGITUDE Surface elevation Ice thickness, glacier Multiple investigations Airborne radio-echo sounding |
description |
Mass changes of polar ice sheets have an important societal impact, because they affect global sea level. Estimating the current mass budget of ice sheets is equivalent to determining the balance between surface mass gain through precipitation and outflow across the grounding line. For the Antarctic ice sheet, grounding line outflow is governed by oceanic processes and outlet glacier dynamics. In this study, we compute the mass budget of major outlet glaciers in the eastern Dronning Maud Land sector of the Antarctic ice sheet using the input/output method. Input is given by recent surface accumulation estimates (SMB) of the whole drainage basin. The outflow at the grounding line is determined from the radar data of a recent airborne survey and satellite-based velocities using a flow model of combined plug flow and simple shear. This approach is an improvement on previous studies, as the ice thickness is measured, rather than being estimated from hydrostatic equilibrium. In line with the general thickening of ... : Geographic coordinates were collected with GPS. Surface elevation is the elevation of the plane (from GPS) corrected for the distance between the plane and the surface measured with laser altimeter. Ice thickness is reconstructed by picking the bed wave on radargram collected with 150-Mhz AWI's airborne radar. The two-way travel time is converted into thickness assuming a constant propagation speed of 168E+006 m/s.These data were collected with the financial support of EUropean Facility for Airborne Research (EUFAR, http://www.eufar.net). ... |
format |
Dataset |
author |
Callens, Denis Matsuoka, Kenichi Steinhage, Daniel Pattyn, Frank |
author_facet |
Callens, Denis Matsuoka, Kenichi Steinhage, Daniel Pattyn, Frank |
author_sort |
Callens, Denis |
title |
Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ... |
title_short |
Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ... |
title_full |
Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ... |
title_fullStr |
Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ... |
title_full_unstemmed |
Surface elevation and ice thickness measurements of an airborne radar survey made in the Sør Rondane Mountains, Antarctica ... |
title_sort |
surface elevation and ice thickness measurements of an airborne radar survey made in the sør rondane mountains, antarctica ... |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://dx.doi.org/10.1594/pangaea.836299 https://doi.pangaea.de/10.1594/PANGAEA.836299 |
genre |
Antarc* Antarctic Antarctica Dronning Maud Land Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Dronning Maud Land Ice Sheet |
op_relation |
https://dx.doi.org/10.3189/2015aog70a010 https://dx.doi.org/10.5194/tc-8-867-2014 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.83629910.3189/2015aog70a01010.5194/tc-8-867-2014 |
_version_ |
1810487212371869696 |