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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Online Access: | http://dx.doi.org/10.1080/16742834.2018.1394779 |
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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 |
work_keys_str_mv |
AT feifeiluo weakerconnectionbetweentheatlanticmultidecadaloscillationandindiansummerrainfallsincethemid1990s AT shuanglinli weakerconnectionbetweentheatlanticmultidecadaloscillationandindiansummerrainfallsincethemid1990s AT torefurevik weakerconnectionbetweentheatlanticmultidecadaloscillationandindiansummerrainfallsincethemid1990s |
_version_ |
1721568674508177408 |