The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones
Abstract Taking advantage of the Polar Amplification Model Intercomparison Project simulations and using a Lagrangian objective feature tracking algorithm, we determine the response of extratropical cyclones to sea‐ice loss and consequent weakening of the equator‐to‐pole near‐surface temperature gra...
Published in: | Geophysical Research Letters |
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Online Access: | https://doi.org/10.1029/2023GL102840 https://doaj.org/article/2d43365637f04b82b568186e1a90237e |
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ftdoajarticles:oai:doaj.org/article:2d43365637f04b82b568186e1a90237e 2024-09-15T18:23:20+00:00 The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones Stephanie Hay Matthew D. K. Priestley Hao Yu Jennifer L. Catto James A. Screen 2023-09-01T00:00:00Z https://doi.org/10.1029/2023GL102840 https://doaj.org/article/2d43365637f04b82b568186e1a90237e EN eng Wiley https://doi.org/10.1029/2023GL102840 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL102840 https://doaj.org/article/2d43365637f04b82b568186e1a90237e Geophysical Research Letters, Vol 50, Iss 17, Pp n/a-n/a (2023) sea ice loss extratropical cyclones midlatitudes Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL102840 2024-08-05T17:49:23Z Abstract Taking advantage of the Polar Amplification Model Intercomparison Project simulations and using a Lagrangian objective feature tracking algorithm, we determine the response of extratropical cyclones to sea‐ice loss and consequent weakening of the equator‐to‐pole near‐surface temperature gradient. The wintertime storm tracks are found to shift equatorward in the North Atlantic and over Europe, and eastward in the North Pacific. In both regions, cyclones become weaker and slower, particularly on the poleward flank of the storm tracks. On average, there are fewer individual cyclones in the extratropics each winter, they last longer, are weaker, and travel more slowly. These changes are greatest over the Arctic, but still statistically significant in midlatitudes despite being small compared to internal variability. Inter‐model spread in cyclone responses are not strongly correlated with that in Arctic warming or Arctic amplification. Little change in summertime cyclones is found. Article in Journal/Newspaper North Atlantic Sea ice Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 17 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
sea ice loss extratropical cyclones midlatitudes Geophysics. Cosmic physics QC801-809 |
spellingShingle |
sea ice loss extratropical cyclones midlatitudes Geophysics. Cosmic physics QC801-809 Stephanie Hay Matthew D. K. Priestley Hao Yu Jennifer L. Catto James A. Screen The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones |
topic_facet |
sea ice loss extratropical cyclones midlatitudes Geophysics. Cosmic physics QC801-809 |
description |
Abstract Taking advantage of the Polar Amplification Model Intercomparison Project simulations and using a Lagrangian objective feature tracking algorithm, we determine the response of extratropical cyclones to sea‐ice loss and consequent weakening of the equator‐to‐pole near‐surface temperature gradient. The wintertime storm tracks are found to shift equatorward in the North Atlantic and over Europe, and eastward in the North Pacific. In both regions, cyclones become weaker and slower, particularly on the poleward flank of the storm tracks. On average, there are fewer individual cyclones in the extratropics each winter, they last longer, are weaker, and travel more slowly. These changes are greatest over the Arctic, but still statistically significant in midlatitudes despite being small compared to internal variability. Inter‐model spread in cyclone responses are not strongly correlated with that in Arctic warming or Arctic amplification. Little change in summertime cyclones is found. |
format |
Article in Journal/Newspaper |
author |
Stephanie Hay Matthew D. K. Priestley Hao Yu Jennifer L. Catto James A. Screen |
author_facet |
Stephanie Hay Matthew D. K. Priestley Hao Yu Jennifer L. Catto James A. Screen |
author_sort |
Stephanie Hay |
title |
The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones |
title_short |
The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones |
title_full |
The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones |
title_fullStr |
The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones |
title_full_unstemmed |
The Effect of Arctic Sea‐Ice Loss on Extratropical Cyclones |
title_sort |
effect of arctic sea‐ice loss on extratropical cyclones |
publisher |
Wiley |
publishDate |
2023 |
url |
https://doi.org/10.1029/2023GL102840 https://doaj.org/article/2d43365637f04b82b568186e1a90237e |
genre |
North Atlantic Sea ice |
genre_facet |
North Atlantic Sea ice |
op_source |
Geophysical Research Letters, Vol 50, Iss 17, Pp n/a-n/a (2023) |
op_relation |
https://doi.org/10.1029/2023GL102840 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL102840 https://doaj.org/article/2d43365637f04b82b568186e1a90237e |
op_doi |
https://doi.org/10.1029/2023GL102840 |
container_title |
Geophysical Research Letters |
container_volume |
50 |
container_issue |
17 |
_version_ |
1810463525993185280 |