Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation

Funding: UK Natural Environment Research Council (NERC) grant NE/N011716/1 (JWBR and AB). Tamaki Foundation, NASA (Grant NNX17AH56G), and NSF (Grant AGS-1929775) (RCJW). NERC Independent Research Fellowship NE/K008536/1 (RFI). North Pacific atmospheric and oceanic circulations are key missing pieces...

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Published in:Geophysical Research Letters
Main Authors: Gray, William Robert, Wills, Robert CJ, Rae, James William Buchanan, Burke, Andrea, Ivanovic, Ruza F, Roberts, William HG, Ferreira, David, Valdes, Paul J
Other Authors: NERC, University of St Andrews. School of Earth & Environmental Sciences, University of St Andrews. St Andrews Isotope Geochemistry
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
DAS
QC
QE
Online Access:http://hdl.handle.net/10023/21638
https://doi.org/10.1029/2019GL086328
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spelling ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/21638 2023-07-02T03:32:36+02:00 Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation Gray, William Robert Wills, Robert CJ Rae, James William Buchanan Burke, Andrea Ivanovic, Ruza F Roberts, William HG Ferreira, David Valdes, Paul J NERC University of St Andrews. School of Earth & Environmental Sciences University of St Andrews. St Andrews Isotope Geochemistry 2021-03-17 application/pdf http://hdl.handle.net/10023/21638 https://doi.org/10.1029/2019GL086328 eng eng Geophysical Research Letters Gray , W R , Wills , R CJ , Rae , J W B , Burke , A , Ivanovic , R F , Roberts , W HG , Ferreira , D & Valdes , P J 2020 , ' Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation ' , Geophysical Research Letters , vol. 47 , no. 6 , e2019GL086328 . https://doi.org/10.1029/2019GL086328 0094-8276 PURE: 266604554 PURE UUID: 59536cf2-40d3-4a79-9607-d58672d1c08e ORCID: /0000-0002-3754-1498/work/70919965 ORCID: /0000-0003-3904-2526/work/70919966 Scopus: 85082527819 WOS: 000529097700012 http://hdl.handle.net/10023/21638 https://doi.org/10.1029/2019GL086328 NE/N011716/1 Copyright © 2020 American Geophysical Union. All Rights Reserved. This work has been made available online in accordance with publisher policies or with permission. Permission for further reuse of this content should be sought from the publisher or the rights holder. This is the final published version of the work, which was originally published at https://doi.org/10.1029/2019GL086328 North Pacific Deglaciation Gyre circulation Westerlies Oxygen isotopes Climate models QC Physics QE Geology DAS SDG 13 - Climate Action QC QE Journal article 2021 ftstandrewserep https://doi.org/10.1029/2019GL086328 2023-06-13T18:29:16Z Funding: UK Natural Environment Research Council (NERC) grant NE/N011716/1 (JWBR and AB). Tamaki Foundation, NASA (Grant NNX17AH56G), and NSF (Grant AGS-1929775) (RCJW). NERC Independent Research Fellowship NE/K008536/1 (RFI). North Pacific atmospheric and oceanic circulations are key missing pieces in our understanding of the reorganisation of the global climate system since the Last Glacial Maximum (LGM). Here, using a basin‐wide compilation of planktic foraminiferal δ18O, we show that the North Pacific subpolar gyre extended ~3° further south during the LGM, consistent with sea surface temperature and productivity proxy data. Climate models indicate that the expansion of the subpolar gyre was associated with a substantial gyre strengthening, and that these gyre circulation changes were driven by a southward shift of the mid‐latitude westerlies and increased wind‐stress from the polar easterlies. Using single‐forcing model runs, we show that these atmospheric circulation changes are a non‐linear response to ice‐sheet topography/albedo, and CO2. Our reconstruction indicates that the gyre boundary (and thus westerly winds) began to migrate northward at ~16.5 ka, driving changes in ocean heat transport, biogeochemistry, and North American hydroclimate. Publisher PDF Peer reviewed Article in Journal/Newspaper Ice Sheet University of St Andrews: Digital Research Repository Pacific Geophysical Research Letters 47 6
institution Open Polar
collection University of St Andrews: Digital Research Repository
op_collection_id ftstandrewserep
language English
topic North Pacific
Deglaciation
Gyre circulation
Westerlies
Oxygen isotopes
Climate models
QC Physics
QE Geology
DAS
SDG 13 - Climate Action
QC
QE
spellingShingle North Pacific
Deglaciation
Gyre circulation
Westerlies
Oxygen isotopes
Climate models
QC Physics
QE Geology
DAS
SDG 13 - Climate Action
QC
QE
Gray, William Robert
Wills, Robert CJ
Rae, James William Buchanan
Burke, Andrea
Ivanovic, Ruza F
Roberts, William HG
Ferreira, David
Valdes, Paul J
Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation
topic_facet North Pacific
Deglaciation
Gyre circulation
Westerlies
Oxygen isotopes
Climate models
QC Physics
QE Geology
DAS
SDG 13 - Climate Action
QC
QE
description Funding: UK Natural Environment Research Council (NERC) grant NE/N011716/1 (JWBR and AB). Tamaki Foundation, NASA (Grant NNX17AH56G), and NSF (Grant AGS-1929775) (RCJW). NERC Independent Research Fellowship NE/K008536/1 (RFI). North Pacific atmospheric and oceanic circulations are key missing pieces in our understanding of the reorganisation of the global climate system since the Last Glacial Maximum (LGM). Here, using a basin‐wide compilation of planktic foraminiferal δ18O, we show that the North Pacific subpolar gyre extended ~3° further south during the LGM, consistent with sea surface temperature and productivity proxy data. Climate models indicate that the expansion of the subpolar gyre was associated with a substantial gyre strengthening, and that these gyre circulation changes were driven by a southward shift of the mid‐latitude westerlies and increased wind‐stress from the polar easterlies. Using single‐forcing model runs, we show that these atmospheric circulation changes are a non‐linear response to ice‐sheet topography/albedo, and CO2. Our reconstruction indicates that the gyre boundary (and thus westerly winds) began to migrate northward at ~16.5 ka, driving changes in ocean heat transport, biogeochemistry, and North American hydroclimate. Publisher PDF Peer reviewed
author2 NERC
University of St Andrews. School of Earth & Environmental Sciences
University of St Andrews. St Andrews Isotope Geochemistry
format Article in Journal/Newspaper
author Gray, William Robert
Wills, Robert CJ
Rae, James William Buchanan
Burke, Andrea
Ivanovic, Ruza F
Roberts, William HG
Ferreira, David
Valdes, Paul J
author_facet Gray, William Robert
Wills, Robert CJ
Rae, James William Buchanan
Burke, Andrea
Ivanovic, Ruza F
Roberts, William HG
Ferreira, David
Valdes, Paul J
author_sort Gray, William Robert
title Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation
title_short Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation
title_full Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation
title_fullStr Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation
title_full_unstemmed Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation
title_sort wind-driven evolution of the north pacific subpolar gyre over the last deglaciation
publishDate 2021
url http://hdl.handle.net/10023/21638
https://doi.org/10.1029/2019GL086328
geographic Pacific
geographic_facet Pacific
genre Ice Sheet
genre_facet Ice Sheet
op_relation Geophysical Research Letters
Gray , W R , Wills , R CJ , Rae , J W B , Burke , A , Ivanovic , R F , Roberts , W HG , Ferreira , D & Valdes , P J 2020 , ' Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation ' , Geophysical Research Letters , vol. 47 , no. 6 , e2019GL086328 . https://doi.org/10.1029/2019GL086328
0094-8276
PURE: 266604554
PURE UUID: 59536cf2-40d3-4a79-9607-d58672d1c08e
ORCID: /0000-0002-3754-1498/work/70919965
ORCID: /0000-0003-3904-2526/work/70919966
Scopus: 85082527819
WOS: 000529097700012
http://hdl.handle.net/10023/21638
https://doi.org/10.1029/2019GL086328
NE/N011716/1
op_rights Copyright © 2020 American Geophysical Union. All Rights Reserved. This work has been made available online in accordance with publisher policies or with permission. Permission for further reuse of this content should be sought from the publisher or the rights holder. This is the final published version of the work, which was originally published at https://doi.org/10.1029/2019GL086328
op_doi https://doi.org/10.1029/2019GL086328
container_title Geophysical Research Letters
container_volume 47
container_issue 6
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