Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming

The Pacific–South America (PSA) teleconnection pattern triggered by the El Niño/Southern Oscillation (ENSO) is suggested to be moving eastward and intensifying under global warming. However, the underlying mechanism is not completely understood. Previous studies have proposed that the movement of th...

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Published in:Frontiers in Earth Science
Main Authors: Ya Wang, Gang Huang, Kaiming Hu, Weichen Tao, Hainan Gong, Kai Yang, Haosu Tang
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2022
Subjects:
Q
Online Access:https://doi.org/10.3389/feart.2022.916624
https://doaj.org/article/22bd083105af4a028326df9cae3f6695
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spelling ftdoajarticles:oai:doaj.org/article:22bd083105af4a028326df9cae3f6695 2023-05-15T13:33:52+02:00 Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming Ya Wang Gang Huang Kaiming Hu Weichen Tao Hainan Gong Kai Yang Haosu Tang 2022-07-01T00:00:00Z https://doi.org/10.3389/feart.2022.916624 https://doaj.org/article/22bd083105af4a028326df9cae3f6695 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/feart.2022.916624/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2022.916624 https://doaj.org/article/22bd083105af4a028326df9cae3f6695 Frontiers in Earth Science, Vol 10 (2022) El Niño/Southern oscillation Global Warming Subtropical Jet Stream Pacific–South American teleconnection pattern ENSO teleconnection Science Q article 2022 ftdoajarticles https://doi.org/10.3389/feart.2022.916624 2022-12-30T21:19:07Z The Pacific–South America (PSA) teleconnection pattern triggered by the El Niño/Southern Oscillation (ENSO) is suggested to be moving eastward and intensifying under global warming. However, the underlying mechanism is not completely understood. Previous studies have proposed that the movement of the PSA teleconnection pattern is attributable to the eastward shift of the tropical Pacific ENSO-driven rainfall anomalies in response to the projected El Niño-like sea surface temperature (SST) warming pattern. In this study, we found that with uniform warming, models will also simulate an eastward movement of the PSA teleconnection pattern, without the impact of the uneven SST warming pattern. Further investigation reveals that future changes in the climatology of the atmospheric circulation, particularly the movement of the exit region of the subtropical jet stream, can also contribute to the eastward shift of the PSA teleconnection pattern by modifying the conversion of mean kinetic energy to eddy kinetic energy. Article in Journal/Newspaper Antarc* Antarctica Directory of Open Access Journals: DOAJ Articles Pacific Frontiers in Earth Science 10
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic El Niño/Southern oscillation
Global Warming
Subtropical Jet Stream
Pacific–South American teleconnection pattern
ENSO teleconnection
Science
Q
spellingShingle El Niño/Southern oscillation
Global Warming
Subtropical Jet Stream
Pacific–South American teleconnection pattern
ENSO teleconnection
Science
Q
Ya Wang
Gang Huang
Kaiming Hu
Weichen Tao
Hainan Gong
Kai Yang
Haosu Tang
Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming
topic_facet El Niño/Southern oscillation
Global Warming
Subtropical Jet Stream
Pacific–South American teleconnection pattern
ENSO teleconnection
Science
Q
description The Pacific–South America (PSA) teleconnection pattern triggered by the El Niño/Southern Oscillation (ENSO) is suggested to be moving eastward and intensifying under global warming. However, the underlying mechanism is not completely understood. Previous studies have proposed that the movement of the PSA teleconnection pattern is attributable to the eastward shift of the tropical Pacific ENSO-driven rainfall anomalies in response to the projected El Niño-like sea surface temperature (SST) warming pattern. In this study, we found that with uniform warming, models will also simulate an eastward movement of the PSA teleconnection pattern, without the impact of the uneven SST warming pattern. Further investigation reveals that future changes in the climatology of the atmospheric circulation, particularly the movement of the exit region of the subtropical jet stream, can also contribute to the eastward shift of the PSA teleconnection pattern by modifying the conversion of mean kinetic energy to eddy kinetic energy.
format Article in Journal/Newspaper
author Ya Wang
Gang Huang
Kaiming Hu
Weichen Tao
Hainan Gong
Kai Yang
Haosu Tang
author_facet Ya Wang
Gang Huang
Kaiming Hu
Weichen Tao
Hainan Gong
Kai Yang
Haosu Tang
author_sort Ya Wang
title Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming
title_short Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming
title_full Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming
title_fullStr Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming
title_full_unstemmed Understanding the Eastward Shift and Intensification of the ENSO Teleconnection Over South Pacific and Antarctica Under Greenhouse Warming
title_sort understanding the eastward shift and intensification of the enso teleconnection over south pacific and antarctica under greenhouse warming
publisher Frontiers Media S.A.
publishDate 2022
url https://doi.org/10.3389/feart.2022.916624
https://doaj.org/article/22bd083105af4a028326df9cae3f6695
geographic Pacific
geographic_facet Pacific
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Frontiers in Earth Science, Vol 10 (2022)
op_relation https://www.frontiersin.org/articles/10.3389/feart.2022.916624/full
https://doaj.org/toc/2296-6463
2296-6463
doi:10.3389/feart.2022.916624
https://doaj.org/article/22bd083105af4a028326df9cae3f6695
op_doi https://doi.org/10.3389/feart.2022.916624
container_title Frontiers in Earth Science
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