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• W1903670331 abstract "[1] In a 46-kyrs' transient accelerated simulation with the NCAR Community Climate System Model version 3 (CCSM3), the increased July insolation at precessional bands causes a drastic summer warming in North Africa, the mid-latitudes of Eurasia from surface to the upper troposphere, with a cooling troposphere in the Northwest Pacific (NWP), which intensifies the land-ocean thermal contrast between Eurasia and its adjacent oceans. Associated with the tropospheric temperature variations are a lower-tropospheric strengthened low-pressure system from North Africa to the mid-high latitudes of Eurasia and a lower-tropospheric strengthened high-pressure system over the NWP. Meanwhile, the strengthened southwesterly or southerly winds prevail over the Asian monsoon region, indicating a stronger Asian summer monsoon. Summer precipitation increases in tropical Africa, South Asia, and the mid-high latitudes of East Asia, with a decreased precipitation over South China and the NWP. This response of atmospheric circulation and monsoon precipitation to the precessional changes is explained in the context of the extratropical Asian-Pacific Oscillation." @default.
• W1903670331 created "2016-06-24" @default.
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• W1903670331 date "2012-07-26" @default.
• W1903670331 modified "2023-10-07" @default.
• W1903670331 title "Extratropical modulation on Asian summer monsoon at precessional bands" @default.
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• W1903670331 doi "https://doi.org/10.1029/2012gl052553" @default.
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