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Relationship between East Asian Monsoon and Dust Weather Frequency over Beijing

Relationship between East Asian Monsoon and Dust Weather Frequency over Beijing

作     者:武云飞 张仁健 韩志伟 曾昭美 WU Yunfei;ZHANG Renjian;HAN Zhiwei;ZENG Zhaomei

作者机构:Key Laboratory of Regional Climate-Environment Research for Temperate East AsiaChinese Academy of Sciences Graduate UniversityChinese Academy of Sciences 

出 版 物:《Advances in Atmospheric Sciences》 (大气科学进展(英文版))

年 卷 期:2010年第27卷第6期

页      面:1389-1398页

核心收录:

学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学] 0816[工学-测绘科学与技术] 0825[工学-航空宇航科学与技术] 

基  金:supported by the Pilot Project of Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-YW-Q11-03) the National Basic Research Program of China(No. 2010CB428503) 

主  题:dust weather frequency East Asian Monsoon correlation 

摘      要:The relationship between dust weather frequency (DWF), which denotes the number of days of dust weather events, over Beijing and the East Asian Monsoon (EAM) was studied using DWF data for Beijing during the period 1951-2006. Results show that, during this period, the blowing-dust weather frequency (BDWF), as well as the indices of East Asian winter monsoon (EAWM) and East Asian summer monsoon (EASM), all decreased considerably, with a t-test confidence level of 99%. The correlation coeffcients between the chosen EAWM index and BDWF over Beijing in winter and the following spring were 0.34 and 0.33, respectively, with significance levels of 0.01 and 0.02, respectively. For the chosen EASM index and BDWF, these correlation coeffcients were 0.51 and 0.45, respectively, with both at a confidence level exceeding 99.9%. With the linear trends removed, the values (in the same order as above) were 0.14, 0.14, -0.12, and -0.09, all not significant at the 95% confidence level. Clearly, the EAM relates mainly to DWF over long timescales. To a certain extent, the EAM might have some impact on DWF by affecting the associated surface air temperature and precipitation during the corresponding time period in sand-dust source regions at the interannual scale. A stronger (weaker) EAWM might advance (suppress) the occurrence of DWF, and the opposite for the EASM.

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