Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry

A decade-long pronounced increase in temperatures in the Arctic, especially in the Barents Sea region, resulted in a global warming hotspot over Svalbard. Associated changes in the cryosphere are the consequence and lead to a demand for monitoring of the glacier changes. This study uses spaceborne l...

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Published in:Remote Sensing
Main Authors: Lukas Sochor, Thorsten Seehaus, Matthias H. Braun
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/rs13112089
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/11/2089/ 2023-08-20T04:04:19+02:00 Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry Lukas Sochor Thorsten Seehaus Matthias H. Braun agris 2021-05-26 application/pdf https://doi.org/10.3390/rs13112089 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs13112089 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 11; Pages: 2089 ICESat ICESat-2 laser altimetry svalbard barents sea geodesy glacier ice cap elevation change mass change Text 2021 ftmdpi https://doi.org/10.3390/rs13112089 2023-08-01T01:48:37Z A decade-long pronounced increase in temperatures in the Arctic, especially in the Barents Sea region, resulted in a global warming hotspot over Svalbard. Associated changes in the cryosphere are the consequence and lead to a demand for monitoring of the glacier changes. This study uses spaceborne laser altimetry data from the ICESat and ICESat-2 missions to obtain ice elevation and mass change rates between 2003–2008 and 2019. Elevation changes are derived at orbit crossover locations throughout the study area, and regional volume and mass changes are estimated using a hypsometric approach. A Svalbard-wide annual elevation change rate of −0.30 ± 0.15 m yr−1 was found, which corresponds to a mass loss rate of −12.40 ± 4.28 Gt yr−1. Compared to the ICESat period (2003–2009), thinning has increased over most regions, including the highest negative rates along the west coast and areas bordering the Barents Sea. The overall negative regime is expected to be linked to Arctic warming in the last decades and associated changes in glacier climatic mass balance. Further, observed increased thinning rates and pronounced changes at the eastern side of Svalbard since the ICESat period are found to correlate with atmospheric and oceanic warming in the respective regions. Text Arctic Barents Sea glacier Global warming Ice cap Svalbard MDPI Open Access Publishing Arctic Svalbard Barents Sea Remote Sensing 13 11 2089
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic ICESat
ICESat-2
laser
altimetry
svalbard
barents sea
geodesy
glacier
ice cap
elevation change
mass change
spellingShingle ICESat
ICESat-2
laser
altimetry
svalbard
barents sea
geodesy
glacier
ice cap
elevation change
mass change
Lukas Sochor
Thorsten Seehaus
Matthias H. Braun
Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry
topic_facet ICESat
ICESat-2
laser
altimetry
svalbard
barents sea
geodesy
glacier
ice cap
elevation change
mass change
description A decade-long pronounced increase in temperatures in the Arctic, especially in the Barents Sea region, resulted in a global warming hotspot over Svalbard. Associated changes in the cryosphere are the consequence and lead to a demand for monitoring of the glacier changes. This study uses spaceborne laser altimetry data from the ICESat and ICESat-2 missions to obtain ice elevation and mass change rates between 2003–2008 and 2019. Elevation changes are derived at orbit crossover locations throughout the study area, and regional volume and mass changes are estimated using a hypsometric approach. A Svalbard-wide annual elevation change rate of −0.30 ± 0.15 m yr−1 was found, which corresponds to a mass loss rate of −12.40 ± 4.28 Gt yr−1. Compared to the ICESat period (2003–2009), thinning has increased over most regions, including the highest negative rates along the west coast and areas bordering the Barents Sea. The overall negative regime is expected to be linked to Arctic warming in the last decades and associated changes in glacier climatic mass balance. Further, observed increased thinning rates and pronounced changes at the eastern side of Svalbard since the ICESat period are found to correlate with atmospheric and oceanic warming in the respective regions.
format Text
author Lukas Sochor
Thorsten Seehaus
Matthias H. Braun
author_facet Lukas Sochor
Thorsten Seehaus
Matthias H. Braun
author_sort Lukas Sochor
title Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry
title_short Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry
title_full Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry
title_fullStr Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry
title_full_unstemmed Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry
title_sort increased ice thinning over svalbard measured by icesat/icesat-2 laser altimetry
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/rs13112089
op_coverage agris
geographic Arctic
Svalbard
Barents Sea
geographic_facet Arctic
Svalbard
Barents Sea
genre Arctic
Barents Sea
glacier
Global warming
Ice cap
Svalbard
genre_facet Arctic
Barents Sea
glacier
Global warming
Ice cap
Svalbard
op_source Remote Sensing; Volume 13; Issue 11; Pages: 2089
op_relation Environmental Remote Sensing
https://dx.doi.org/10.3390/rs13112089
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs13112089
container_title Remote Sensing
container_volume 13
container_issue 11
container_start_page 2089
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