Summer monsoon in Southeast Asia can cause large-scale precipitation in the region in early summer, which is featured by prevailing low-level southwesterly from the Bay of Bengal to South China Sea （SCS）. It has cha...Summer monsoon in Southeast Asia can cause large-scale precipitation in the region in early summer, which is featured by prevailing low-level southwesterly from the Bay of Bengal to South China Sea （SCS）. It has characteristics of its own as well as those of Asian monsoons in general. As found in studies over recent years on East Asian monsoons, the earliest onset of the Southeast Asian summer monsoon occurs in early summer over the SCS, among all members of the monsoon system. It then advances westward to India and northward to eastern China, Japan and Korean Peninsula. As pointed out by Lau and Yang121, the end of April is the earliest time when the Asian monsoon sets up at the southern tip of Indo-china Peninsula. Being the earliest signal for the whole summer monsoon system in Asia, it may be of some predictive value for the establishment of Asian summer monsoon （ASM）.展开更多
Based on daily NCEP reanalysis data, OLR and satellite rainfall data, the characteristic of theactivities of South China Sea summer monsoon(SCSSM) in 2004 were analyzed. The results showed that theestablishment of SCS...Based on daily NCEP reanalysis data, OLR and satellite rainfall data, the characteristic of theactivities of South China Sea summer monsoon(SCSSM) in 2004 were analyzed. The results showed that theestablishment of SCSSM was little later than normal and the intensity was stronger than normal. Influenced bythe location of the northwest Pacific subtropical high, which was much northward and westward than normal,SCSSM was active mainly in the South China Sea areas. There existed obvious intraseasonal oscillation and twosignificant periods of SCSSM, one was about 20-30 days and the other about 40-50 days. The transportation ofmoisture was concentrated on the South China Sea and the northwest Pacific regions, reducing the northwardtransportation and resulting in drought in southern China.展开更多
文摘Summer monsoon in Southeast Asia can cause large-scale precipitation in the region in early summer, which is featured by prevailing low-level southwesterly from the Bay of Bengal to South China Sea （SCS）. It has characteristics of its own as well as those of Asian monsoons in general. As found in studies over recent years on East Asian monsoons, the earliest onset of the Southeast Asian summer monsoon occurs in early summer over the SCS, among all members of the monsoon system. It then advances westward to India and northward to eastern China, Japan and Korean Peninsula. As pointed out by Lau and Yang121, the end of April is the earliest time when the Asian monsoon sets up at the southern tip of Indo-china Peninsula. Being the earliest signal for the whole summer monsoon system in Asia, it may be of some predictive value for the establishment of Asian summer monsoon （ASM）.
基金Public Well-being Research Project from the Ministry of Science and Technology(2002RKT01)Natural Science Foundation of Guangdong Province (04003915)Natural Science Foundation ofChina (90211010)
文摘Based on daily NCEP reanalysis data, OLR and satellite rainfall data, the characteristic of theactivities of South China Sea summer monsoon(SCSSM) in 2004 were analyzed. The results showed that theestablishment of SCSSM was little later than normal and the intensity was stronger than normal. Influenced bythe location of the northwest Pacific subtropical high, which was much northward and westward than normal,SCSSM was active mainly in the South China Sea areas. There existed obvious intraseasonal oscillation and twosignificant periods of SCSSM, one was about 20-30 days and the other about 40-50 days. The transportation ofmoisture was concentrated on the South China Sea and the northwest Pacific regions, reducing the northwardtransportation and resulting in drought in southern China.
