1) monsoon onset
季风暴发
1.
On the basis of the CTD observation data obtained by the two cruises before and after Asian monsoon onset (25th, May 1998, several significant hydrographic characteristics distribution of the South China Sea (SCS), its variation and formation mechanism are analyzed.
利用1998年亚洲季风暴发(5月25日)前后的两次CTD观测,分析了季风暴发前后南海若干重要水文特征分布、变化及其形成机制。
2) Outbreak in summer
夏季暴发
3) westerly wind burst
西风暴发
1.
The re- sults show that the eastward transport of warm water of the western tropical Pacific due to the westerly wind burst leads not only to a drop of sea level but also to a rise of thermocline in the western tropic.
本文利用“ＣｌｉｍａｔｅＤｉａｇｎｏｓｔｉｃｓＢｕｌｌｅｔｉｎ”、“ＯｃｅａｎｏｇｒａｐｈｉｃＭｏｎｔｈｌｙＳｕｍ－ｍａｒｙ”、美国夏威夷水位中心提供的资料以及ＴＯＧＡ－ＣＯＡＲＥＩＯＰ资料，分析了１９９２～１９９３厄尔尼诺事件中西太平洋暖池、东太平洋ＳＳＴ对异常风场的响应，结果指出：由于西风暴发而引起的西太平洋暖水向东输送，不仅导致西太平详水位降低，而且导致温跃层显著升高，进而引起上层海水热含量显著减少，这种减少在温跃层更为明显。
2.
Westerly wind bursts can influence the sea water movement in different layers.
提出两次西风暴发过程中流场的变化:第一次西风暴发之后,流场形成稳定的东向流,位相有10d的滞后(包括开始与结束);第二次西风暴发之后,流场迅速变为东向流,第一次西风暴发强度比第二次强,但是,第一次西风暴发过程中流速却低于第二次。
4) monsoon onset
季风爆发
1.
Diurnal cycle of marine atmospheric boundary layer during the 1998 summer monsoon onset over South China Sea
1998年季风爆发期南海大气边界层的日变化
2.
By using the 1950-1999 NCEP daily averaged reanalyzed data and based on the major atmosphere characteristics at 850 hPa during southwest monsoon onset in the South China Sea (SCS), it is suggested an objective atmospheric circulation way to define the onset dates of SCS southwest monsoon.
利用1950～1999年NCEP全球格点日平均资料,在总结南海西南季风爆发前后850hPa大气环流特征的基础上,提出了一个较为客观的确定南海西南季风爆发日期的大气环流方法。
3.
Based on the NCEP/NCAR reanalysis datasets,the influence of anomalous diabatic heating over the Tibetan Plateau(TP) in spring on the Asian tropical monsoon onset were investigated by performing composite analysis.
使用NCEP/NCAR再分析等资料,从年际变化的角度,选取季风爆发前青藏高原感热加热异常强/弱年进行合成分析,结果表明:季风爆发前高原加热异常偏强,使得高层环流趋向于季节变化的方向;中、低层孟加拉湾等地区有气旋式环流、上升运动及降水增强,孟加拉湾季风爆发偏早。
5) summer monsoon onset
夏季风爆发
1.
Vihma, and the relation between the dynamic and thermodynamic features of upper mixed layer and the summer monsoon onset.
Ｖｉｈｍａ提出的方法，计算了潜热通量、感热通量和风应力，分析了南海上 混合层动力、热力特征及其与南海夏季风爆发之间的关系。
6) Westerly Wind Burst Event (WWBE)
西风暴发事件(WWBE)
补充资料：季风(见季风气候)
季风(见季风气候)
j!feng候季风见季风气
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条