Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean
Abstract The Arctic Ocean is projected to become seasonally ice‐free before midcentury unless greenhouse gas emissions are rapidly reduced, but exactly when this could occur depends considerably on internal climate variability. Here we show that trajectories to an ice‐free Arctic are modulated by co...
Published in: | Geophysical Research Letters |
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Online Access: | https://doi.org/10.1029/2018GL081393 https://doaj.org/article/ac1beffc03e54f7d8e4443dbf21a8020 |
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ftdoajarticles:oai:doaj.org/article:ac1beffc03e54f7d8e4443dbf21a8020 2024-09-09T18:56:49+00:00 Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean J. A. Screen C. Deser 2019-02-01T00:00:00Z https://doi.org/10.1029/2018GL081393 https://doaj.org/article/ac1beffc03e54f7d8e4443dbf21a8020 EN eng Wiley https://doi.org/10.1029/2018GL081393 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2018GL081393 https://doaj.org/article/ac1beffc03e54f7d8e4443dbf21a8020 Geophysical Research Letters, Vol 46, Iss 4, Pp 2222-2231 (2019) Arctic sea ice climate variability Interdecadal Pacific Oscillation large ensemble climate projections teleconnection Geophysics. Cosmic physics QC801-809 article 2019 ftdoajarticles https://doi.org/10.1029/2018GL081393 2024-08-05T17:49:10Z Abstract The Arctic Ocean is projected to become seasonally ice‐free before midcentury unless greenhouse gas emissions are rapidly reduced, but exactly when this could occur depends considerably on internal climate variability. Here we show that trajectories to an ice‐free Arctic are modulated by concomitant shifts in the Interdecadal Pacific Oscillation (IPO). Trajectories starting in the negative IPO phase become ice‐free 7 years sooner than those starting in the positive IPO phase. Trajectories starting in the negative IPO phase subsequently transition toward the positive IPO phase, on average, with an associated strengthening of the Aleutian Low, increased poleward energy transport, and faster sea‐ice loss. The observed IPO began to transition away from its negative phase in the past few years. If this shift continues, our results suggest increased likelihood of accelerated sea‐ice loss over the coming decades, and an increased risk of an ice‐free Arctic within the next 20–30 years. Article in Journal/Newspaper aleutian low Arctic Arctic Ocean Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Pacific Geophysical Research Letters 46 4 2222 2231 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic sea ice climate variability Interdecadal Pacific Oscillation large ensemble climate projections teleconnection Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Arctic sea ice climate variability Interdecadal Pacific Oscillation large ensemble climate projections teleconnection Geophysics. Cosmic physics QC801-809 J. A. Screen C. Deser Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean |
topic_facet |
Arctic sea ice climate variability Interdecadal Pacific Oscillation large ensemble climate projections teleconnection Geophysics. Cosmic physics QC801-809 |
description |
Abstract The Arctic Ocean is projected to become seasonally ice‐free before midcentury unless greenhouse gas emissions are rapidly reduced, but exactly when this could occur depends considerably on internal climate variability. Here we show that trajectories to an ice‐free Arctic are modulated by concomitant shifts in the Interdecadal Pacific Oscillation (IPO). Trajectories starting in the negative IPO phase become ice‐free 7 years sooner than those starting in the positive IPO phase. Trajectories starting in the negative IPO phase subsequently transition toward the positive IPO phase, on average, with an associated strengthening of the Aleutian Low, increased poleward energy transport, and faster sea‐ice loss. The observed IPO began to transition away from its negative phase in the past few years. If this shift continues, our results suggest increased likelihood of accelerated sea‐ice loss over the coming decades, and an increased risk of an ice‐free Arctic within the next 20–30 years. |
format |
Article in Journal/Newspaper |
author |
J. A. Screen C. Deser |
author_facet |
J. A. Screen C. Deser |
author_sort |
J. A. Screen |
title |
Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean |
title_short |
Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean |
title_full |
Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean |
title_fullStr |
Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean |
title_full_unstemmed |
Pacific Ocean Variability Influences the Time of Emergence of a Seasonally Ice‐Free Arctic Ocean |
title_sort |
pacific ocean variability influences the time of emergence of a seasonally ice‐free arctic ocean |
publisher |
Wiley |
publishDate |
2019 |
url |
https://doi.org/10.1029/2018GL081393 https://doaj.org/article/ac1beffc03e54f7d8e4443dbf21a8020 |
geographic |
Arctic Arctic Ocean Pacific |
geographic_facet |
Arctic Arctic Ocean Pacific |
genre |
aleutian low Arctic Arctic Ocean Sea ice |
genre_facet |
aleutian low Arctic Arctic Ocean Sea ice |
op_source |
Geophysical Research Letters, Vol 46, Iss 4, Pp 2222-2231 (2019) |
op_relation |
https://doi.org/10.1029/2018GL081393 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2018GL081393 https://doaj.org/article/ac1beffc03e54f7d8e4443dbf21a8020 |
op_doi |
https://doi.org/10.1029/2018GL081393 |
container_title |
Geophysical Research Letters |
container_volume |
46 |
container_issue |
4 |
container_start_page |
2222 |
op_container_end_page |
2231 |
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1809819903274778624 |