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Contribution of tropical cyclone rainfall at categories to total precipitation over the Western North Pacific from 1998 to 2007

Contribution of tropical cyclone rainfall at categories to total precipitation over the Western North Pacific from 1998 to 2007

作     者:CHEN FengJiao FU YunFei 

作者机构:School of Earth and Space Sciences University of Science and Technology of China State Key Laboratory of Severe Weather Chinese Academy of Meteorological Sciences 

出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))

年 卷 期:2015年第58卷第11期

页      面:2015-2025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] 

基  金:supported by the Special Funds for Public Welfare of China(Grant No.GYHY201306077) CAS Strategic Priority Research Program(Grant No.XDA05100303) the National Natural Science Foundation of China(Grant Nos.41230419,91337213) the Jiangsu Provincial 2011 Program(Collaborative Innovation Center of Climate Change) 

主  题:tropical cyclone precipitation contribution 3B42 WNP ENSO 

摘      要:Based on 10 years precipitation data from Tropical Rainfall Measurement Mission (TRMM) Multi-satellite Precipitation Analysis (TMPA) 3B42 and the best track data from China Meteorological Administration (CMA), the seasonal, monthly and annual contribution of tropical cyclone (TC) precipitation to the total rainfall are analyzed over the Western North Pacific (WNP) during 1998 to 2007 from May to December. The results show that: (1) TC seasonal rainfall contribution ranges from 4% in inland regions to above 40% in ocean-regions of 15°N-25°N. TCs at higher categories contribute much more to the total precipitation. (2) On monthly scale, TCs contribute 60% to the total rainfall regionally during whole TC season, which is the maximum contribution. The peak contribution of TC rainfall averaged in multi-months of the ten years occurs in August (28%) over the whole ocean impacted by TC and in December (23%) over the whole land impacted by TC, respectively. (3) On annual scale, the maximum contribution of TC precipitation to the total rainfall are in 2004 (-30%) over ocean and in 1998 (-20%) over land, respectively. (4) The contribution of TC precipitation to the total rainfall increases 6% (decreases 6%) in El Nino (La Nifia) years compared with neutral years.

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