Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990s

Previous studies have shown that the Atlantic Multidecadal Oscillation (AMO) can play an important role in modulating the variability of Indian summer monsoon rainfall (ISMR) over a 50–60-yr timescale. A significant positive correlation between the AMO and ISMR is found both in observations and mode...

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Main Authors: Fei-Fei LUO, Shuanglin LI, Tore FUREVIK
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2018-01-01
Series:Atmospheric and Oceanic Science Letters
Subjects:
Online Access:http://dx.doi.org/10.1080/16742834.2018.1394779
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spelling doaj-fd1228ed84504db19ef73073802c8ef72021-04-02T12:32:53ZengKeAi Communications Co., Ltd.Atmospheric and Oceanic Science Letters1674-28342376-61232018-01-01111374310.1080/16742834.2018.13947791394779Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990sFei-Fei LUO0Shuanglin LI1Tore FUREVIK2Chinese Academy of SciencesChinese Academy of SciencesUniversity of BergenPrevious studies have shown that the Atlantic Multidecadal Oscillation (AMO) can play an important role in modulating the variability of Indian summer monsoon rainfall (ISMR) over a 50–60-yr timescale. A significant positive correlation between the AMO and ISMR is found both in observations and models. However, instrumental records show that the relationship becomes non-significant or even of opposite sign after the mid-1990s, suggesting a weakening of the AMO–ISMR connection. The mechanism for the breakdown of the AMO–ISMR connection is investigated in the present work, and the results suggest that a substantial warming in the Indian–tropical western Pacific Ocean plays a role. The warming weakens the meridional gradient of tropospheric temperature between Eurasia and the Indian Ocean, and reduces the meridional sea level pressure gradient between the Indian Subcontinent and Indian Ocean, weakening the Indian summer monsoon. Thus, warming in the Indian–tropical western Pacific Ocean seems responsible for the weakened connection between the AMO and ISM.http://dx.doi.org/10.1080/16742834.2018.1394779Atlantic Multidecadal OscillationIndian summer rainfallconnectionmultidecadal variation
collection DOAJ
language English
format Article
sources DOAJ
author Fei-Fei LUO
Shuanglin LI
Tore FUREVIK
spellingShingle Fei-Fei LUO
Shuanglin LI
Tore FUREVIK
Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990s
Atmospheric and Oceanic Science Letters
Atlantic Multidecadal Oscillation
Indian summer rainfall
connection
multidecadal variation
author_facet Fei-Fei LUO
Shuanglin LI
Tore FUREVIK
author_sort Fei-Fei LUO
title Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990s
title_short Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990s
title_full Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990s
title_fullStr Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990s
title_full_unstemmed Weaker connection between the Atlantic Multidecadal Oscillation and Indian summer rainfall since the mid-1990s
title_sort weaker connection between the atlantic multidecadal oscillation and indian summer rainfall since the mid-1990s
publisher KeAi Communications Co., Ltd.
series Atmospheric and Oceanic Science Letters
issn 1674-2834
2376-6123
publishDate 2018-01-01
description Previous studies have shown that the Atlantic Multidecadal Oscillation (AMO) can play an important role in modulating the variability of Indian summer monsoon rainfall (ISMR) over a 50–60-yr timescale. A significant positive correlation between the AMO and ISMR is found both in observations and models. However, instrumental records show that the relationship becomes non-significant or even of opposite sign after the mid-1990s, suggesting a weakening of the AMO–ISMR connection. The mechanism for the breakdown of the AMO–ISMR connection is investigated in the present work, and the results suggest that a substantial warming in the Indian–tropical western Pacific Ocean plays a role. The warming weakens the meridional gradient of tropospheric temperature between Eurasia and the Indian Ocean, and reduces the meridional sea level pressure gradient between the Indian Subcontinent and Indian Ocean, weakening the Indian summer monsoon. Thus, warming in the Indian–tropical western Pacific Ocean seems responsible for the weakened connection between the AMO and ISM.
topic Atlantic Multidecadal Oscillation
Indian summer rainfall
connection
multidecadal variation
url http://dx.doi.org/10.1080/16742834.2018.1394779
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