Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica

Abstract The Antarctic ice sheet (AIS) is the largest freshwater body on Earth and a major component of the sea level budget. Over the satellite era, the AIS has experienced ∼130 Gt/year of mass loss. Net losses are partially mitigated by snow accumulation that varies ∼100–130 Gt/yr, underscoring a...

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Published in:Geophysical Research Letters
Main Authors: Jessica D. Kromer, Luke D. Trusel
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL104436
https://doaj.org/article/d9c7a9b86e6e4460835fb2e60703c2b7
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spelling ftdoajarticles:oai:doaj.org/article:d9c7a9b86e6e4460835fb2e60703c2b7 2024-09-15T17:39:02+00:00 Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica Jessica D. Kromer Luke D. Trusel 2023-09-01T00:00:00Z https://doi.org/10.1029/2023GL104436 https://doaj.org/article/d9c7a9b86e6e4460835fb2e60703c2b7 EN eng Wiley https://doi.org/10.1029/2023GL104436 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL104436 https://doaj.org/article/d9c7a9b86e6e4460835fb2e60703c2b7 Geophysical Research Letters, Vol 50, Iss 18, Pp n/a-n/a (2023) West Antarctic surface mass balance sea ice variability snowfall Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL104436 2024-08-05T17:49:23Z Abstract The Antarctic ice sheet (AIS) is the largest freshwater body on Earth and a major component of the sea level budget. Over the satellite era, the AIS has experienced ∼130 Gt/year of mass loss. Net losses are partially mitigated by snow accumulation that varies ∼100–130 Gt/yr, underscoring a need to understand the drivers of snowfall variability. Here, we evaluate impacts of decreased sea ice in the Amundsen Sea region of West Antarctica on the overlying atmosphere and surface mass balance of the adjacent AIS using composites, spatial correlations, and a causal effect network method. Importantly, our findings show sea ice declines in the Amundsen Sea lead to enhanced integrated water vapor that is subsequently transported to the AIS resulting in positive anomalies in West Antarctic ice sheet snowfall. Our results suggest future decreases in sea ice may likely enhance ice sheet snowfall, thus partially offsetting Antarctic sea level contributions. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Antarctica Ice Sheet Sea ice West Antarctica Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 18
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic West Antarctic
surface mass balance
sea ice variability
snowfall
Geophysics. Cosmic physics
QC801-809
spellingShingle West Antarctic
surface mass balance
sea ice variability
snowfall
Geophysics. Cosmic physics
QC801-809
Jessica D. Kromer
Luke D. Trusel
Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica
topic_facet West Antarctic
surface mass balance
sea ice variability
snowfall
Geophysics. Cosmic physics
QC801-809
description Abstract The Antarctic ice sheet (AIS) is the largest freshwater body on Earth and a major component of the sea level budget. Over the satellite era, the AIS has experienced ∼130 Gt/year of mass loss. Net losses are partially mitigated by snow accumulation that varies ∼100–130 Gt/yr, underscoring a need to understand the drivers of snowfall variability. Here, we evaluate impacts of decreased sea ice in the Amundsen Sea region of West Antarctica on the overlying atmosphere and surface mass balance of the adjacent AIS using composites, spatial correlations, and a causal effect network method. Importantly, our findings show sea ice declines in the Amundsen Sea lead to enhanced integrated water vapor that is subsequently transported to the AIS resulting in positive anomalies in West Antarctic ice sheet snowfall. Our results suggest future decreases in sea ice may likely enhance ice sheet snowfall, thus partially offsetting Antarctic sea level contributions.
format Article in Journal/Newspaper
author Jessica D. Kromer
Luke D. Trusel
author_facet Jessica D. Kromer
Luke D. Trusel
author_sort Jessica D. Kromer
title Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica
title_short Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica
title_full Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica
title_fullStr Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica
title_full_unstemmed Identifying the Impacts of Sea Ice Variability on the Climate and Surface Mass Balance of West Antarctica
title_sort identifying the impacts of sea ice variability on the climate and surface mass balance of west antarctica
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL104436
https://doaj.org/article/d9c7a9b86e6e4460835fb2e60703c2b7
genre Amundsen Sea
Antarc*
Antarctic
Antarctica
Ice Sheet
Sea ice
West Antarctica
genre_facet Amundsen Sea
Antarc*
Antarctic
Antarctica
Ice Sheet
Sea ice
West Antarctica
op_source Geophysical Research Letters, Vol 50, Iss 18, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL104436
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL104436
https://doaj.org/article/d9c7a9b86e6e4460835fb2e60703c2b7
op_doi https://doi.org/10.1029/2023GL104436
container_title Geophysical Research Letters
container_volume 50
container_issue 18
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