Thermodynamic and dynamic effects on regional monsoon rainfall changes in a warmer climate
نویسندگان
چکیده
منابع مشابه
Delayed Seasonal Cycle and African Monsoon in a Warmer Climate
Increasing greenhouse gases will change many aspects of the Earth’s climate, from its annual mean to the frequency of extremes such as heat waves and droughts[1]. Here we report that the current generation of climate models predicts a delay in the seasonal cycle of global rainfall and ocean temperature in response to increasing greenhouse gases, with important implications for the regional mons...
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[1] Key climate feedback due to water vapor and clouds rest largely on how relative humidity R changes in a warmer climate, yet this has not been extensively analyzed in models. General circulation models (GCMs) from the CMIP3 archive and several higher‐ resolution atmospheric GCMs examined here generally predict a characteristic pattern of R trend with global temperature that has been reported...
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The response of East Asian Summer Monsoon (EASM) precipitation to long term changes in regional anthropogenic aerosols (sulphate and black carbon) is explored in an atmospheric general circulation model, the atmospheric component of the UK High-Resolution Global Environment Model v1.2 (HiGAM). Separately, sulphur dioxide (SO2) and black carbon (BC) emissions in 1950 and 2000 over East Asia are ...
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It is well known that the sea surface temperature (hereafter, referred to as SST) is a critical component which influences the exchange of energy between the atmosphere and ocean. Since SST influences atmosphere as well as is controlled by atmospheric conditions, accurate SST data from observation or predicted by model plays a crucial role in weather forecast and research. However, the spatial ...
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ژورنال
عنوان ژورنال: Geophysical Research Letters
سال: 2014
ISSN: 0094-8276
DOI: 10.1002/2013gl059158