Seasonal response of Asian monsoonal climate to the Atlantic Multidecadal Oscillation

The influence of the Atlantic Multidecadal Oscillation (AMO) on Asian monsoonal climate in all four seasons is investigated by comprehensive observational analyses and ensemble experiments with atmospheric general circulation models (AGCMs). Three AGCMs are forced by prescribed climatological season...

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Published inJournal of Geophysical Research: Atmospheres Vol. 114; no. D2
Main Authors Wang, Yanming, Li, Shuanglin, Luo, Dehai
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 27.01.2009
American Geophysical Union
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Abstract The influence of the Atlantic Multidecadal Oscillation (AMO) on Asian monsoonal climate in all four seasons is investigated by comprehensive observational analyses and ensemble experiments with atmospheric general circulation models (AGCMs). Three AGCMs are forced by prescribed climatological seasonal cycle of sea surface temperature (SST) or with additional SST anomalies representing the warmth phase of the AMO. The results in both the observations and the models consistently suggest that the warm AMO phase gives rise to elevated air temperatures in East Asia and northern India but decreased air temperatures in much of central‐southern India in all four seasons. This positive AMO anomaly also causes more rainfall in central and southern India in every season, particularly in summer and fall. In contrast, the sign of AMO influences on East Asian rainfall is season‐dependent: in southeastern China, it induces increased rainfall in summer but suppressed rainfall in autumn. It is suggested that these AMO influences are realized by warming Eurasian middle and upper troposphere in all four seasons, resulting in weakened Asian winter monsoons but enhanced summer monsoons. Furthermore, the formation of the troposphere heating anomaly may be related to the wave guidance mechanism associated with the Asian upper jet.
AbstractList The influence of the Atlantic Multidecadal Oscillation (AMO) on Asian monsoonal climate in all four seasons is investigated by comprehensive observational analyses and ensemble experiments with atmospheric general circulation models (AGCMs). Three AGCMs are forced by prescribed climatological seasonal cycle of sea surface temperature (SST) or with additional SST anomalies representing the warmth phase of the AMO. The results in both the observations and the models consistently suggest that the warm AMO phase gives rise to elevated air temperatures in East Asia and northern India but decreased air temperatures in much of central-southern India in all four seasons. This positive AMO anomaly also causes more rainfall in central and southern India in every season, particularly in summer and fall. In contrast, the sign of AMO influences on East Asian rainfall is season-dependent: in southeastern China, it induces increased rainfall in summer but suppressed rainfall in autumn. It is suggested that these AMO influences are realized by warming Eurasian middle and upper troposphere in all four seasons, resulting in weakened Asian winter monsoons but enhanced summer monsoons. Furthermore, the formation of the troposphere heating anomaly may be related to the wave guidance mechanism associated with the Asian upper jet.
Author Luo, Dehai
Li, Shuanglin
Wang, Yanming
Author_xml – sequence: 1
  givenname: Yanming
  surname: Wang
  fullname: Wang, Yanming
  organization: College of Physical and Environmental Oceanography, Ocean University of China, Qingdao, China
– sequence: 2
  givenname: Shuanglin
  surname: Li
  fullname: Li, Shuanglin
  email: shuanglin.li@mail.iap.ac.cn
  organization: Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
– sequence: 3
  givenname: Dehai
  surname: Luo
  fullname: Luo, Dehai
  organization: College of Physical and Environmental Oceanography, Ocean University of China, Qingdao, China
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Atmosphere model
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atmospheric precipitation
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Sea surface temperature
troposphere
anomalies
Winter monsoon
Summer monsoon
Atlantic multidecadal oscillation
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seasonal variations
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Snippet The influence of the Atlantic Multidecadal Oscillation (AMO) on Asian monsoonal climate in all four seasons is investigated by comprehensive observational...
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SubjectTerms Anomalies
Asian
Asian monsoonal climate
Atlantic Multidecadal Oscillation
Earth sciences
Earth, ocean, space
Exact sciences and technology
Marine
Monsoons
Oscillations
Rainfall
Seasons
Summer
surface temperature
Troposphere
Title Seasonal response of Asian monsoonal climate to the Atlantic Multidecadal Oscillation
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https://onlinelibrary.wiley.com/doi/abs/10.1029%2F2008JD010929
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Volume 114
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