Zonal propagation of kinetic energy and convection in the South China Sea and Indian monsoon regions in boreal summer
Zonal propagation of kinetic energy (KE) and convection in the South China Sea (SCS) and Indian summer monsoon areas are examined in present study. Results suggest that the SCS and Indian summer monsoon prevailed regions (5-15°N) are dominated by the southwesterly wind, however, the disturbances of KE at 850 hPa and convection are observed mainly coming from the western Pacific Ocean (140-150°E), after passing through the SCS, and westward propagated into the Bay of Bengal (90-100°E). In the Indian summer monsoon domain, where the disturbances of KE are found mainly coming from the Arabian Sea (AS) and eastward propagated into the Bay of Bengal. Therefore, the SCS and the Indian summer monsoon are quite different in zonal propagation of KE and convection. The SCS summer monsoon is mainly affected by the KE and convection coming from the tropical western Pacific. The Indian summer monsoon, however, can be partly influenced by the AS and the SCS summer monsoon. The analysis also suggests that the interaction region between the SCS and the Indian summer monsoon is around 90-95°E, rather than 105°E as proposed by earlier studies.
作 者： Chen Longxun GAO Hui HE Jinhai Tao Shiyan JIN Zuhui 作者单位： Chen Longxun(Chinese Academy of Meteorological Sciences, Beijing 100081, China)GAO Hui,HE Jinhai(Nanjing Institute of Meteorology, Nanjing 210044, China)
Tao Shiyan,JIN Zuhui(Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China)
刊 名： 中国科学D辑（英文版） SCI 英文刊名： SCIENCE IN CHINA SERIES D 年，卷(期)： 2004 47(12) 分类号： P4 关键词： zonal propagation of KE and convection East Asian monsoon Indian monsoon