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...

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Published in:Geophysical Research Letters
Main Authors: Stephanie Hay, Matthew D. K. Priestley, Hao Yu, Jennifer L. Catto, James A. Screen
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL102840
https://doaj.org/article/2d43365637f04b82b568186e1a90237e
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spelling 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
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