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(duì)流增強(qiáng)期間,蘇門(mén)答臘南部地區(qū)對(duì)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(shí)間是5月第4候，爆發(fā)的時(shí)間和強(qiáng)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(cè)1998年南海夏季風(fēng)爆發(fā)的時(shí)間和強(qiáng)度與實(shí)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(qiáng)度還與爆發(fā)期間大氣對(duì)流的30-60天振蕩到達(dá)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、向外長(zhǎng)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(dòng)的一些特徵。