Spatially heterogeneous effect of climate warming on the Arctic land ice

Global warming has already substantially altered the Arctic cryosphere. Due to the Arctic warming amplification, the temperature is increasing more strongly, leading to pervasive changes in this area. Recent years were notably marked by melt records over the Greenland Ice Sheet, while other regions...

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Published in:The Cryosphere
Main Authors: Maure, Damien, Kittel, Christoph, Lambin, Clara, Delhasse, Alison, Fettweis, Xavier
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-4645-2023
https://tc.copernicus.org/articles/17/4645/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc109160 2023-12-10T09:44:18+01:00 Spatially heterogeneous effect of climate warming on the Arctic land ice Maure, Damien Kittel, Christoph Lambin, Clara Delhasse, Alison Fettweis, Xavier 2023-11-06 application/pdf https://doi.org/10.5194/tc-17-4645-2023 https://tc.copernicus.org/articles/17/4645/2023/ eng eng doi:10.5194/tc-17-4645-2023 https://tc.copernicus.org/articles/17/4645/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-4645-2023 2023-11-13T17:24:18Z Global warming has already substantially altered the Arctic cryosphere. Due to the Arctic warming amplification, the temperature is increasing more strongly, leading to pervasive changes in this area. Recent years were notably marked by melt records over the Greenland Ice Sheet, while other regions such as Svalbard seem to remain less influenced. This raises the question of the current state of the Greenland Ice Sheet and the various ice caps in the Arctic for which few studies are available. Here, we run the regional climate model (RCM) Modèle Atmosphérique Régional (MAR) at a resolution of 6 km over four different domains covering all Arctic land ice to produce a unified surface mass balance product from 1950 to the present day. We also compare our results to large-scale indices to better understand the heterogeneity of the evolutions across the Arctic and their links to recent climate change. We find a sharp decrease of surface mass balance (SMB) over the western Arctic (Canada and Greenland) in relationship with the atmospheric blocking situations that have become more frequent in summer, resulting in a 41 % increase of the melt rate since 1950. This increase is not seen over the Russian Arctic permanent ice areas, where melt rates have increased by only 3 % on average, illustrating a heterogeneity in the Arctic SMB response to global warming. Text arctic cryosphere Arctic Climate change Global warming Greenland Ice Sheet Svalbard Copernicus Publications: E-Journals Arctic Canada Greenland Svalbard The Cryosphere 17 11 4645 4659
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Global warming has already substantially altered the Arctic cryosphere. Due to the Arctic warming amplification, the temperature is increasing more strongly, leading to pervasive changes in this area. Recent years were notably marked by melt records over the Greenland Ice Sheet, while other regions such as Svalbard seem to remain less influenced. This raises the question of the current state of the Greenland Ice Sheet and the various ice caps in the Arctic for which few studies are available. Here, we run the regional climate model (RCM) Modèle Atmosphérique Régional (MAR) at a resolution of 6 km over four different domains covering all Arctic land ice to produce a unified surface mass balance product from 1950 to the present day. We also compare our results to large-scale indices to better understand the heterogeneity of the evolutions across the Arctic and their links to recent climate change. We find a sharp decrease of surface mass balance (SMB) over the western Arctic (Canada and Greenland) in relationship with the atmospheric blocking situations that have become more frequent in summer, resulting in a 41 % increase of the melt rate since 1950. This increase is not seen over the Russian Arctic permanent ice areas, where melt rates have increased by only 3 % on average, illustrating a heterogeneity in the Arctic SMB response to global warming.
format Text
author Maure, Damien
Kittel, Christoph
Lambin, Clara
Delhasse, Alison
Fettweis, Xavier
spellingShingle Maure, Damien
Kittel, Christoph
Lambin, Clara
Delhasse, Alison
Fettweis, Xavier
Spatially heterogeneous effect of climate warming on the Arctic land ice
author_facet Maure, Damien
Kittel, Christoph
Lambin, Clara
Delhasse, Alison
Fettweis, Xavier
author_sort Maure, Damien
title Spatially heterogeneous effect of climate warming on the Arctic land ice
title_short Spatially heterogeneous effect of climate warming on the Arctic land ice
title_full Spatially heterogeneous effect of climate warming on the Arctic land ice
title_fullStr Spatially heterogeneous effect of climate warming on the Arctic land ice
title_full_unstemmed Spatially heterogeneous effect of climate warming on the Arctic land ice
title_sort spatially heterogeneous effect of climate warming on the arctic land ice
publishDate 2023
url https://doi.org/10.5194/tc-17-4645-2023
https://tc.copernicus.org/articles/17/4645/2023/
geographic Arctic
Canada
Greenland
Svalbard
geographic_facet Arctic
Canada
Greenland
Svalbard
genre arctic cryosphere
Arctic
Climate change
Global warming
Greenland
Ice Sheet
Svalbard
genre_facet arctic cryosphere
Arctic
Climate change
Global warming
Greenland
Ice Sheet
Svalbard
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-4645-2023
https://tc.copernicus.org/articles/17/4645/2023/
op_doi https://doi.org/10.5194/tc-17-4645-2023
container_title The Cryosphere
container_volume 17
container_issue 11
container_start_page 4645
op_container_end_page 4659
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