Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic

Abstract West Antarctic and the Antarctic Peninsula have experienced dramatic warming in austral spring since the 1970s. Using observations and the Community Atmosphere Model version 4 (CAM4), this study explores the physical mechanism by which the tropical Pacific and Indian Ocean temperature anoma...

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Published in:npj Climate and Atmospheric Science
Main Authors: Ping Zhang, Anmin Duan
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Online Access:https://doi.org/10.1038/s41612-023-00381-8
https://doaj.org/article/a3788e10733942e882b6587daafd4ce6
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spelling ftdoajarticles:oai:doaj.org/article:a3788e10733942e882b6587daafd4ce6 2023-06-18T03:35:55+02:00 Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic Ping Zhang Anmin Duan 2023-05-01T00:00:00Z https://doi.org/10.1038/s41612-023-00381-8 https://doaj.org/article/a3788e10733942e882b6587daafd4ce6 EN eng Nature Portfolio https://doi.org/10.1038/s41612-023-00381-8 https://doaj.org/toc/2397-3722 doi:10.1038/s41612-023-00381-8 2397-3722 https://doaj.org/article/a3788e10733942e882b6587daafd4ce6 npj Climate and Atmospheric Science, Vol 6, Iss 1, Pp 1-9 (2023) Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1038/s41612-023-00381-8 2023-06-04T00:40:34Z Abstract West Antarctic and the Antarctic Peninsula have experienced dramatic warming in austral spring since the 1970s. Using observations and the Community Atmosphere Model version 4 (CAM4), this study explores the physical mechanism by which the tropical Pacific and Indian Ocean temperature anomaly mode (PIM) affects the dipolar surface air temperature (SAT) anomalies across the West Antarctic in austral spring. The positive phase of the PIM, characterized by positive sea surface temperature anomalies (SSTAs) in the tropical central-eastern Pacific and western Indian Ocean and negative SSTAs in the Maritime Continent, can generate two branches of stationary Rossby wave trains propagating from the tropical central Pacific and southeastern Indian Ocean to the West Antarctic, with an anticyclonic anomaly appearing over the Amundsen Sea. The northerlies advect warmer air to the Ross–Amundsen Seas, but southerlies advect colder air to the Antarctic Peninsula–Weddell Sea, resulting in the dipole of SAT anomalies over the West Antarctic. In this process, the role of tropical central-eastern Pacific SSTAs dominate, and it is amplified by the SSTAs around the Maritime Continent. The SSTAs in the western Indian Ocean combined with the SSTAs over the Maritime Continent further contribute to the western pole of the SAT. Only simulation that includes a prescribed PIM forcing can exactly reproduce the observations of the dipolar SAT response across the West Antarctic, indicating the need to treat the tropical Pacific and Indian Oceans as a unified whole. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Antarctic Peninsula Weddell Sea Directory of Open Access Journals: DOAJ Articles Amundsen Sea Antarctic Antarctic Peninsula Austral Indian Pacific The Antarctic Weddell Weddell Sea npj Climate and Atmospheric Science 6 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Ping Zhang
Anmin Duan
Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic
topic_facet Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Abstract West Antarctic and the Antarctic Peninsula have experienced dramatic warming in austral spring since the 1970s. Using observations and the Community Atmosphere Model version 4 (CAM4), this study explores the physical mechanism by which the tropical Pacific and Indian Ocean temperature anomaly mode (PIM) affects the dipolar surface air temperature (SAT) anomalies across the West Antarctic in austral spring. The positive phase of the PIM, characterized by positive sea surface temperature anomalies (SSTAs) in the tropical central-eastern Pacific and western Indian Ocean and negative SSTAs in the Maritime Continent, can generate two branches of stationary Rossby wave trains propagating from the tropical central Pacific and southeastern Indian Ocean to the West Antarctic, with an anticyclonic anomaly appearing over the Amundsen Sea. The northerlies advect warmer air to the Ross–Amundsen Seas, but southerlies advect colder air to the Antarctic Peninsula–Weddell Sea, resulting in the dipole of SAT anomalies over the West Antarctic. In this process, the role of tropical central-eastern Pacific SSTAs dominate, and it is amplified by the SSTAs around the Maritime Continent. The SSTAs in the western Indian Ocean combined with the SSTAs over the Maritime Continent further contribute to the western pole of the SAT. Only simulation that includes a prescribed PIM forcing can exactly reproduce the observations of the dipolar SAT response across the West Antarctic, indicating the need to treat the tropical Pacific and Indian Oceans as a unified whole.
format Article in Journal/Newspaper
author Ping Zhang
Anmin Duan
author_facet Ping Zhang
Anmin Duan
author_sort Ping Zhang
title Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic
title_short Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic
title_full Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic
title_fullStr Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic
title_full_unstemmed Connection between the Tropical Pacific and Indian Ocean and Temperature Anomaly across West Antarctic
title_sort connection between the tropical pacific and indian ocean and temperature anomaly across west antarctic
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41612-023-00381-8
https://doaj.org/article/a3788e10733942e882b6587daafd4ce6
geographic Amundsen Sea
Antarctic
Antarctic Peninsula
Austral
Indian
Pacific
The Antarctic
Weddell
Weddell Sea
geographic_facet Amundsen Sea
Antarctic
Antarctic Peninsula
Austral
Indian
Pacific
The Antarctic
Weddell
Weddell Sea
genre Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Weddell Sea
genre_facet Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Weddell Sea
op_source npj Climate and Atmospheric Science, Vol 6, Iss 1, Pp 1-9 (2023)
op_relation https://doi.org/10.1038/s41612-023-00381-8
https://doaj.org/toc/2397-3722
doi:10.1038/s41612-023-00381-8
2397-3722
https://doaj.org/article/a3788e10733942e882b6587daafd4ce6
op_doi https://doi.org/10.1038/s41612-023-00381-8
container_title npj Climate and Atmospheric Science
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