Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019

The melting of the polar ice caps is considered to be an essential factor for global sea-level rise and has received significant attention. Quantitative research on ice cap mass changes is critical in global climate change. In this study, GRACE JPL RL06 data under the Mascon scheme based on the dyna...

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Published in:Remote Sensing
Main Authors: Yaqiong Mu, Yanqiang Wei, Jinkui Wu, Yongjian Ding, Donghui Shangguan, Di Zeng
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/rs12162609
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spelling ftmdpi:oai:mdpi.com:/2072-4292/12/16/2609/ 2023-08-20T04:04:41+02:00 Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019 Yaqiong Mu Yanqiang Wei Jinkui Wu Yongjian Ding Donghui Shangguan Di Zeng agris 2020-08-13 application/pdf https://doi.org/10.3390/rs12162609 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs12162609 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 12; Issue 16; Pages: 2609 ice sheet change climate change GRACE gravity satellite Arctic region Text 2020 ftmdpi https://doi.org/10.3390/rs12162609 2023-07-31T23:55:23Z The melting of the polar ice caps is considered to be an essential factor for global sea-level rise and has received significant attention. Quantitative research on ice cap mass changes is critical in global climate change. In this study, GRACE JPL RL06 data under the Mascon scheme based on the dynamic method were used. Greenland, which is highly sensitive to climate change, was selected as the study area. Greenland was divided into six sub-research regions, according to its watersheds. The spatial–temporal mass changes were compared to corresponding temperature and precipitation statistics to analyze the relationship between changes in ice sheet mass and climate change. The results show that: (i) From February 2002 to September 2019, the rate of change in the Greenland Ice Sheet mass was about −263 ± 13 Gt yr−1 and the areas with the most substantial ice sheet loss and climate changes were concentrated in the western and southern parts of Greenland. (ii) The mass balance of the Greenland Ice Sheet during the study period was at a loss, and this was closely related to increasing trends in temperature and precipitation. (iii) In the coastal areas of western and southern Greenland, the rate of mass change has accelerated significantly, mainly because of climate change. Text Arctic Climate change Greenland Ice cap Ice Sheet MDPI Open Access Publishing Arctic Greenland Remote Sensing 12 16 2609
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic ice sheet change
climate change
GRACE gravity satellite
Arctic region
spellingShingle ice sheet change
climate change
GRACE gravity satellite
Arctic region
Yaqiong Mu
Yanqiang Wei
Jinkui Wu
Yongjian Ding
Donghui Shangguan
Di Zeng
Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019
topic_facet ice sheet change
climate change
GRACE gravity satellite
Arctic region
description The melting of the polar ice caps is considered to be an essential factor for global sea-level rise and has received significant attention. Quantitative research on ice cap mass changes is critical in global climate change. In this study, GRACE JPL RL06 data under the Mascon scheme based on the dynamic method were used. Greenland, which is highly sensitive to climate change, was selected as the study area. Greenland was divided into six sub-research regions, according to its watersheds. The spatial–temporal mass changes were compared to corresponding temperature and precipitation statistics to analyze the relationship between changes in ice sheet mass and climate change. The results show that: (i) From February 2002 to September 2019, the rate of change in the Greenland Ice Sheet mass was about −263 ± 13 Gt yr−1 and the areas with the most substantial ice sheet loss and climate changes were concentrated in the western and southern parts of Greenland. (ii) The mass balance of the Greenland Ice Sheet during the study period was at a loss, and this was closely related to increasing trends in temperature and precipitation. (iii) In the coastal areas of western and southern Greenland, the rate of mass change has accelerated significantly, mainly because of climate change.
format Text
author Yaqiong Mu
Yanqiang Wei
Jinkui Wu
Yongjian Ding
Donghui Shangguan
Di Zeng
author_facet Yaqiong Mu
Yanqiang Wei
Jinkui Wu
Yongjian Ding
Donghui Shangguan
Di Zeng
author_sort Yaqiong Mu
title Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019
title_short Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019
title_full Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019
title_fullStr Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019
title_full_unstemmed Variations of Mass Balance of the Greenland Ice Sheet from 2002 to 2019
title_sort variations of mass balance of the greenland ice sheet from 2002 to 2019
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/rs12162609
op_coverage agris
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Climate change
Greenland
Ice cap
Ice Sheet
genre_facet Arctic
Climate change
Greenland
Ice cap
Ice Sheet
op_source Remote Sensing; Volume 12; Issue 16; Pages: 2609
op_relation Environmental Remote Sensing
https://dx.doi.org/10.3390/rs12162609
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs12162609
container_title Remote Sensing
container_volume 12
container_issue 16
container_start_page 2609
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