Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study

In this paper, results of diagnostic analysis for the period 1983–2015, demonstrate a robust relationship between Indian Summer Monsoon Rainfall (ISMR) and sea ice area (SIA) over the two sectors of Antarctica namely, Western Pacific Ocean (WPO) and Bellingshausen and Amundsen Seas (BAS). A signific...

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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16881
http://id.nii.ac.jp/1291/00016750/
id ftnipr:oai:nipr.repo.nii.ac.jp:00016881
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00016881 2023-05-15T13:46:39+02:00 Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study 2021-12 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16881 http://id.nii.ac.jp/1291/00016750/ en eng https://doi.org/10.1016/j.polar.2021.100746 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16881 http://id.nii.ac.jp/1291/00016750/ Polar Science, 30, 100746(2021-12) 18739652 Antarctic sea ice WPO and BAS sectors Pacific SST ISMR El Niño Modoki Journal Article 2021 ftnipr https://doi.org/10.1016/j.polar.2021.100746 2023-02-18T20:11:55Z In this paper, results of diagnostic analysis for the period 1983–2015, demonstrate a robust relationship between Indian Summer Monsoon Rainfall (ISMR) and sea ice area (SIA) over the two sectors of Antarctica namely, Western Pacific Ocean (WPO) and Bellingshausen and Amundsen Seas (BAS). A significant direct (inverse) relationship is observed between ISMR and SIA over the WPO (BAS) sector. Further, plausible physical mechanism governing this relationship is proposed. El Niño Modoki exhibit direct (inverse) relation with SIA over BAS (WPO) sector during summer monsoon season, which has prompted investigation of SIA-El Niño Modoki-ISMR connection. The linkage between southern polar sea ice and the Indian summer monsoon has been demonstrated through the Pacific Ocean, wherein above normal SIA over the BAS (WPO) sector is associated with concurrent warm equatorial central (western) Pacific Sea Surface Temperature (SST) anomalies. Associated meridional circulations supplemented by above normal BAS (WPO) SIA extremes is accompanied by an ascending motion over the equatorial central (western) Pacific. In turn, through large-scale zonal circulation, ascending branch of circulation over the central (western) Pacific Ocean contemporaneously impacts ISMR adversely (favourably). Large-scale atmospheric circulation modulated by equatorial Pacific SST signature is suggested as a possible link between Antarctic sea ice and ISMR. Article in Journal/Newspaper Antarc* Antarctic Antarctica Polar Science Polar Science Sea ice National Institute of Polar Research Repository, Japan Antarctic Pacific Indian Polar Science 30 100746
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Antarctic sea ice
WPO and BAS sectors
Pacific SST
ISMR
El Niño Modoki
spellingShingle Antarctic sea ice
WPO and BAS sectors
Pacific SST
ISMR
El Niño Modoki
Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study
topic_facet Antarctic sea ice
WPO and BAS sectors
Pacific SST
ISMR
El Niño Modoki
description In this paper, results of diagnostic analysis for the period 1983–2015, demonstrate a robust relationship between Indian Summer Monsoon Rainfall (ISMR) and sea ice area (SIA) over the two sectors of Antarctica namely, Western Pacific Ocean (WPO) and Bellingshausen and Amundsen Seas (BAS). A significant direct (inverse) relationship is observed between ISMR and SIA over the WPO (BAS) sector. Further, plausible physical mechanism governing this relationship is proposed. El Niño Modoki exhibit direct (inverse) relation with SIA over BAS (WPO) sector during summer monsoon season, which has prompted investigation of SIA-El Niño Modoki-ISMR connection. The linkage between southern polar sea ice and the Indian summer monsoon has been demonstrated through the Pacific Ocean, wherein above normal SIA over the BAS (WPO) sector is associated with concurrent warm equatorial central (western) Pacific Sea Surface Temperature (SST) anomalies. Associated meridional circulations supplemented by above normal BAS (WPO) SIA extremes is accompanied by an ascending motion over the equatorial central (western) Pacific. In turn, through large-scale zonal circulation, ascending branch of circulation over the central (western) Pacific Ocean contemporaneously impacts ISMR adversely (favourably). Large-scale atmospheric circulation modulated by equatorial Pacific SST signature is suggested as a possible link between Antarctic sea ice and ISMR.
format Article in Journal/Newspaper
title Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study
title_short Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study
title_full Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study
title_fullStr Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study
title_full_unstemmed Association between Antarctic Sea ice, Pacific SST and the Indian summer monsoon: An observational study
title_sort association between antarctic sea ice, pacific sst and the indian summer monsoon: an observational study
publishDate 2021
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16881
http://id.nii.ac.jp/1291/00016750/
geographic Antarctic
Pacific
Indian
geographic_facet Antarctic
Pacific
Indian
genre Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
Sea ice
op_relation https://doi.org/10.1016/j.polar.2021.100746
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16881
http://id.nii.ac.jp/1291/00016750/
Polar Science, 30, 100746(2021-12)
18739652
op_doi https://doi.org/10.1016/j.polar.2021.100746
container_title Polar Science
container_volume 30
container_start_page 100746
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