Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s

IntroductionA subdecadal (i.e. , three-year running mean) variation over the tropical Pacific is very distinctively observed in the 2000s.Results and methodsHere, we have demonstrated that sea surface temperature (SST) anomalies in the tropical Atlantic contribute to forming high ocean-temperature a...

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Published in:Frontiers in Climate
Main Authors: Takashi Mochizuki, Masahiro Watanabe
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2022
Subjects:
Online Access:https://doi.org/10.3389/fclim.2022.1040352
https://doaj.org/article/1668a3f09a0c48b3813ed7396fc8b128
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spelling ftdoajarticles:oai:doaj.org/article:1668a3f09a0c48b3813ed7396fc8b128 2023-05-15T17:33:09+02:00 Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s Takashi Mochizuki Masahiro Watanabe 2022-11-01T00:00:00Z https://doi.org/10.3389/fclim.2022.1040352 https://doaj.org/article/1668a3f09a0c48b3813ed7396fc8b128 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fclim.2022.1040352/full https://doaj.org/toc/2624-9553 2624-9553 doi:10.3389/fclim.2022.1040352 https://doaj.org/article/1668a3f09a0c48b3813ed7396fc8b128 Frontiers in Climate, Vol 4 (2022) subdecadal variability interbasin connection walker circulation ocean thermocline tropical climate partial data assimilation Environmental sciences GE1-350 article 2022 ftdoajarticles https://doi.org/10.3389/fclim.2022.1040352 2022-12-30T21:15:41Z IntroductionA subdecadal (i.e. , three-year running mean) variation over the tropical Pacific is very distinctively observed in the 2000s.Results and methodsHere, we have demonstrated that sea surface temperature (SST) anomalies in the tropical Atlantic contribute to forming high ocean-temperature anomalies in the tropical Pacific in the early 2000s by performing partial data assimilation of a global climate model. Low SSTs over the equatorial Atlantic change the Walker circulation, and the associated weakening of the Pacific trade winds raises the equatorial SST on subdecadal timescales. At the same time, a high SST anomaly is also generated in the off-equatorial North Pacific through deepening of the upper ocean thermocline due to an accompanying anticyclonic surface wind anomaly aloft. While the subtropical North Atlantic SSTs may help the subdecadal warming in the equatorial Pacific, the resultant SST anomalies show a one-year delay in the phase transition and are modestly accompanied by ocean thermocline deepening.DiscussionIt roughly follows the IMRaD format. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Pacific Frontiers in Climate 4
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic subdecadal variability
interbasin connection
walker circulation
ocean thermocline
tropical climate
partial data assimilation
Environmental sciences
GE1-350
spellingShingle subdecadal variability
interbasin connection
walker circulation
ocean thermocline
tropical climate
partial data assimilation
Environmental sciences
GE1-350
Takashi Mochizuki
Masahiro Watanabe
Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s
topic_facet subdecadal variability
interbasin connection
walker circulation
ocean thermocline
tropical climate
partial data assimilation
Environmental sciences
GE1-350
description IntroductionA subdecadal (i.e. , three-year running mean) variation over the tropical Pacific is very distinctively observed in the 2000s.Results and methodsHere, we have demonstrated that sea surface temperature (SST) anomalies in the tropical Atlantic contribute to forming high ocean-temperature anomalies in the tropical Pacific in the early 2000s by performing partial data assimilation of a global climate model. Low SSTs over the equatorial Atlantic change the Walker circulation, and the associated weakening of the Pacific trade winds raises the equatorial SST on subdecadal timescales. At the same time, a high SST anomaly is also generated in the off-equatorial North Pacific through deepening of the upper ocean thermocline due to an accompanying anticyclonic surface wind anomaly aloft. While the subtropical North Atlantic SSTs may help the subdecadal warming in the equatorial Pacific, the resultant SST anomalies show a one-year delay in the phase transition and are modestly accompanied by ocean thermocline deepening.DiscussionIt roughly follows the IMRaD format.
format Article in Journal/Newspaper
author Takashi Mochizuki
Masahiro Watanabe
author_facet Takashi Mochizuki
Masahiro Watanabe
author_sort Takashi Mochizuki
title Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s
title_short Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s
title_full Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s
title_fullStr Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s
title_full_unstemmed Atlantic impacts on subdecadal warming over the tropical Pacific in the 2000s
title_sort atlantic impacts on subdecadal warming over the tropical pacific in the 2000s
publisher Frontiers Media S.A.
publishDate 2022
url https://doi.org/10.3389/fclim.2022.1040352
https://doaj.org/article/1668a3f09a0c48b3813ed7396fc8b128
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Frontiers in Climate, Vol 4 (2022)
op_relation https://www.frontiersin.org/articles/10.3389/fclim.2022.1040352/full
https://doaj.org/toc/2624-9553
2624-9553
doi:10.3389/fclim.2022.1040352
https://doaj.org/article/1668a3f09a0c48b3813ed7396fc8b128
op_doi https://doi.org/10.3389/fclim.2022.1040352
container_title Frontiers in Climate
container_volume 4
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