SCSSM

基本解釋

Before( during) the SCSSM sets up, the convection over the south of Sumatra area thrives( weakens).
南海地區(qū)對流增強期間,囌門答臘南部地區(qū)對流減弱。
The main results are as follows.The mean onset time of SCSSM is the fourth pentad of May for the period 1980 to 1991.
結(jié)果表明：南海夏季風(fēng)爆發(fā)平均時間是5月第4候，爆發(fā)的時間和強度有顯著的年際變化，爆發(fā)期間的海氣狀況與大氣的低頻振蕩密切相關(guān)。
Prediction of the onset of 1998" SCSSM based on SST during the prior period in SCS is consistent with the real fact.
根據(jù)前期南海海溫預(yù)測1998年南海夏季風(fēng)爆發(fā)的時間和強度與實況相符。
The strength of SCSSM is also related to the phase of 30-60 day oscillation of TBB arrived over SCS during the onset period of SCSSM.
它爆發(fā)的強度還與爆發(fā)期間大氣對流的30-60天振蕩到達南海的位相有關(guān)；
Based on daily NCEP reanalysis data, OLR and satellite rainfall data, the characteristic of the activities of South China Sea summer monsoon (SCSSM) in 2004 were analyzed.
摘要利用NCEP逐日再分析資料、曏外長波輻射(OLR)和衛(wèi)星降水資料，分析了2004年影響南海夏季風(fēng)活動的一些特徵。