Projected changes of Greenland’s periphery glaciers and ice caps

Rapid global warming has caused drastic mass loss in Greenland’s peripheral glaciers and ice caps (GICs), contributing to a rise of global sea levels. To better understand future changes under different emission scenarios, we used the Open Global Glacier Model to simulate glacier dynamics and runoff...

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Main Authors: Limin Kang, Minghu Ding, Yuzhe Wang, Weijun Sun, Lei Wang, Hongmin An, Qinglin Zhang, Jiahang Che, Baojuan Huai
Format: Article
Language:English
Published: IOP Publishing 2024-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ad8b5f
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author Limin Kang
Minghu Ding
Yuzhe Wang
Weijun Sun
Lei Wang
Hongmin An
Qinglin Zhang
Jiahang Che
Baojuan Huai
author_facet Limin Kang
Minghu Ding
Yuzhe Wang
Weijun Sun
Lei Wang
Hongmin An
Qinglin Zhang
Jiahang Che
Baojuan Huai
author_sort Limin Kang
collection DOAJ
description Rapid global warming has caused drastic mass loss in Greenland’s peripheral glaciers and ice caps (GICs), contributing to a rise of global sea levels. To better understand future changes under different emission scenarios, we used the Open Global Glacier Model to simulate glacier dynamics and runoff changes from 2015 to 2100. The results show that their area and volume will decrease by 38.88% (SSP1-2.6) to 60.84% (SSP5-8.5) and 47.56% (SSP1-2.6) to 67.10% (SSP5-8.5) by 2100, with regions that have larger glacierized areas and are farther from the ocean experiencing less volume loss. Meanwhile, the predicted surface mass balance of Greenland’s peripheral GICs in 2100 is −0.58 ± 0.92, −1.18 ± 1.13, −2.04 ± 0.79 and −3.16 ± 0.96 m w.e. a ^−1 under four emission scenarios. The runoff under higher emission scenarios is larger than that under lower emission scenarios, with peak water occurring later in regions that have larger glacierized areas and are farther from the ocean.
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issn 1748-9326
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publishDate 2024-01-01
publisher IOP Publishing
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series Environmental Research Letters
spelling doaj-art-87bbf832d6ac4dacbb7cad6565f5bcdb2024-11-12T15:16:08ZengIOP PublishingEnvironmental Research Letters1748-93262024-01-01191212404110.1088/1748-9326/ad8b5fProjected changes of Greenland’s periphery glaciers and ice capsLimin Kang0https://orcid.org/0009-0000-7167-801XMinghu Ding1https://orcid.org/0000-0002-1142-6598Yuzhe Wang2https://orcid.org/0000-0003-3564-6787Weijun Sun3https://orcid.org/0000-0002-6386-8937Lei Wang4https://orcid.org/0000-0003-4742-7127Hongmin An5https://orcid.org/0000-0002-3412-295XQinglin Zhang6https://orcid.org/0000-0001-8048-951XJiahang Che7https://orcid.org/0000-0003-1698-5679Baojuan Huai8https://orcid.org/0000-0002-1415-8234College of Geography and Environment, Shandong Normal University , Jinan 250358, People’s Republic of ChinaState Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences , Beijing 100081, People’s Republic of ChinaCollege of Geography and Environment, Shandong Normal University , Jinan 250358, People’s Republic of ChinaCollege of Geography and Environment, Shandong Normal University , Jinan 250358, People’s Republic of ChinaCollege of Geography and Environment, Shandong Normal University , Jinan 250358, People’s Republic of ChinaCollege of Geography and Environment, Shandong Normal University , Jinan 250358, People’s Republic of ChinaState Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences , Beijing 100081, People’s Republic of ChinaCollege of Geography and Environment, Shandong Normal University , Jinan 250358, People’s Republic of ChinaCollege of Geography and Environment, Shandong Normal University , Jinan 250358, People’s Republic of ChinaRapid global warming has caused drastic mass loss in Greenland’s peripheral glaciers and ice caps (GICs), contributing to a rise of global sea levels. To better understand future changes under different emission scenarios, we used the Open Global Glacier Model to simulate glacier dynamics and runoff changes from 2015 to 2100. The results show that their area and volume will decrease by 38.88% (SSP1-2.6) to 60.84% (SSP5-8.5) and 47.56% (SSP1-2.6) to 67.10% (SSP5-8.5) by 2100, with regions that have larger glacierized areas and are farther from the ocean experiencing less volume loss. Meanwhile, the predicted surface mass balance of Greenland’s peripheral GICs in 2100 is −0.58 ± 0.92, −1.18 ± 1.13, −2.04 ± 0.79 and −3.16 ± 0.96 m w.e. a ^−1 under four emission scenarios. The runoff under higher emission scenarios is larger than that under lower emission scenarios, with peak water occurring later in regions that have larger glacierized areas and are farther from the ocean.https://doi.org/10.1088/1748-9326/ad8b5fGreenlandGICsOGGMCMIP6projections
spellingShingle Limin Kang
Minghu Ding
Yuzhe Wang
Weijun Sun
Lei Wang
Hongmin An
Qinglin Zhang
Jiahang Che
Baojuan Huai
Projected changes of Greenland’s periphery glaciers and ice caps
Environmental Research Letters
Greenland
GICs
OGGM
CMIP6
projections
title Projected changes of Greenland’s periphery glaciers and ice caps
title_full Projected changes of Greenland’s periphery glaciers and ice caps
title_fullStr Projected changes of Greenland’s periphery glaciers and ice caps
title_full_unstemmed Projected changes of Greenland’s periphery glaciers and ice caps
title_short Projected changes of Greenland’s periphery glaciers and ice caps
title_sort projected changes of greenland s periphery glaciers and ice caps
topic Greenland
GICs
OGGM
CMIP6
projections
url https://doi.org/10.1088/1748-9326/ad8b5f
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