Diurnal Cycle and Propagation of Convection over South China Coastal Region during Mei-Yu Season
Introduction The diurnal cycle is one of the most fundamental modes in the earth climate system.Characterizing the diurnal cycle and propagation of convective storms can help us understand not only the initiation and evolution mechanism of convection but also the mechanism that drives the local climate.In recent years, diurnal cycle of precipitation in China,especially during the warm season also received much attention based on surface, radar and satellite observations (e.g.,Chen et al.2014a; Xu and Zipser 2011; Yu et al.2010).During the warm season, there are three rainfall centers or maximum rainfall regions in China: South China, Yangtze-Huai River Basin and North China (Ding and Chan 2005).Convective rainfall is believed to be the major contributor to the total warm season precipitation in these three regions(e.g., Liu and Fu 2010; Luo et al.2012).
Kun Zhao Xingchao Chen Ming Xue Fuqing Zhang
国内会议
北京
英文
90-94
2015-12-01（万方平台首次上网日期，不代表论文的发表时间）