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《Chinese Journal of Atmospheric Sciences》 2006-01
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Climatic Variations of Wet Days in China

WANG Ying~(1),SHI Neng~(1,2),GU Jun-Qiang ~(3),FENG Guo-Lin~(4),and ZHANG Li-Bo~(1)1 Key Laboratory of Meteorology and Environment,Nanjing University of Information Science and Technology,Nanjing 210044 2 Guangzhou Institute of Tropical and oceanic Meteorology,Guangzhou 5100083 Meteorological Science Research Institute of Zhejiang Province,Hangzhou 3100174 Key Laboratory of Climate Research,National Climate Center,Beijing 100081  
There have been many studies on climatic changes in rainfall and droughts/floods,however,study on climatic changes in wet days has been rarely seen.The wet day number of a place is associated with rainfall in the place,but differs from the rainfall.The existing studies show that changes in wet day number differ from those in rainfall.It is necessary to study changes in wet day number,especially to study the difference between them,under the global warming.Up to now,study on climatic changes in wet days nation-wide has not been seen.The climatic change of wet days and the spatial/temporal features of annual,seasonal,and monthly wet days in China are investigated in the context of the observational data at 160 stations during the period of 19542000 by using modern statistical diagnostic methods such as the computation of trend coefficients.It is pointed out that the annual wet days have declined at a mean rate of 3.8 days per decade,and the decline of wet days is more obvious than that of rainfall.The temporal trends of seasonal wet days are all negative with a mean reduction rate of one day per decade.The reduction of summer wet days is most remarkable(most statistically significant),and the reduction of autumn wet days is the largest in magnitude.As far as the spatial change of the secular trend variation of annual wet days is concerned,the reduction of annual wet days is the largest in Northeast China,North China and Southwest China,where the reduction rate is 710 days per decade.The secular trend variation of wet days does not completely accord with that of rainfall.The negative trend of annual wet days not only covers a larger area than the negative trend of rainfall,but its intensity is also larger,i.e.,the absolute value of the negative trend is larger.The distinct negative trend of annual rainfall lies only in North China within(34°N38°N,109°E122°E),while the largest reduction of annual wet days covers Northeast China,North China,Southwest China,which is a larger area than North China.The secular trend variation of seasonal wet days differs greatly from that of seasonal rainfall.The seasonal wet days do not show an obviously positive trend in a single season at a single station.However,the seasonal rainfall shows a negative trend only in autumn over a large-scale area,but an evident positive trend in summer at some stations.In winter,the seasonal rainfall shows a negative trend only over a small area(the winter precipitation is increasing in China).In Northeast China,the winter rainfall is reducing only over a small area,but the wet day is reducing evidently over a large-scale area.
【Fund】: 国家自然科学基金资助项目40275028、90411008
【CateGory Index】: P467
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