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: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Q
Online Access:https://doi.org/10.3390/rs13112089
https://doaj.org/article/02cd17906d5e48cda56a33156e93a6aa
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spelling ftdoajarticles:oai:doaj.org/article:02cd17906d5e48cda56a33156e93a6aa 2023-05-15T14:57:43+02:00 Increased Ice Thinning over Svalbard Measured by ICESat/ICESat-2 Laser Altimetry Lukas Sochor Thorsten Seehaus Matthias H. Braun 2021-05-01T00:00:00Z https://doi.org/10.3390/rs13112089 https://doaj.org/article/02cd17906d5e48cda56a33156e93a6aa EN eng MDPI AG https://www.mdpi.com/2072-4292/13/11/2089 https://doaj.org/toc/2072-4292 doi:10.3390/rs13112089 2072-4292 https://doaj.org/article/02cd17906d5e48cda56a33156e93a6aa Remote Sensing, Vol 13, Iss 2089, p 2089 (2021) ICESat ICESat-2 laser altimetry svalbard barents sea Science Q article 2021 ftdoajarticles https://doi.org/10.3390/rs13112089 2022-12-31T16:18:31Z 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. Article in Journal/Newspaper Arctic Barents Sea glacier Global warming Svalbard Directory of Open Access Journals: DOAJ Articles Arctic Barents Sea Svalbard Remote Sensing 13 11 2089
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic ICESat
ICESat-2
laser
altimetry
svalbard
barents sea
Science
Q
spellingShingle ICESat
ICESat-2
laser
altimetry
svalbard
barents sea
Science
Q
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
Science
Q
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 Article in Journal/Newspaper
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 MDPI AG
publishDate 2021
url https://doi.org/10.3390/rs13112089
https://doaj.org/article/02cd17906d5e48cda56a33156e93a6aa
geographic Arctic
Barents Sea
Svalbard
geographic_facet Arctic
Barents Sea
Svalbard
genre Arctic
Barents Sea
glacier
Global warming
Svalbard
genre_facet Arctic
Barents Sea
glacier
Global warming
Svalbard
op_source Remote Sensing, Vol 13, Iss 2089, p 2089 (2021)
op_relation https://www.mdpi.com/2072-4292/13/11/2089
https://doaj.org/toc/2072-4292
doi:10.3390/rs13112089
2072-4292
https://doaj.org/article/02cd17906d5e48cda56a33156e93a6aa
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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