2) SCS summer monsoon onset
南海夏季风爆发
1.
Influences of SSTA over Kuroshio on SCS summer monsoon onset and the western Pacific subtropical high from April to June are investigated.
采用合成分析和相关分析等方法讨论了季节转换时期 ( 4～ 6月 )黑潮地区海温异常对南海夏季风爆发时间和西太平洋副高位置与强度的影响。
3) South China Sea monsoon onset
南海季风爆发
1.
The characteristics of the surface temperature deviation in East Asia-Tropical Eastern Indian Ocean and its relation to the South China Sea monsoon onset is analyzed by EOF technique.
对５月东亚至热带东印度洋表面温度距平主要特征向量场的分析表明，以苏门答腊为中心的热带海洋温度异常与南海季风爆发有密切关系。
4) onset of South China Sea summer monsoon
南海夏季风爆发
1.
Multi-year JEDAC data of heat content in upper ocean and NCEP/NCAR reanalysis data were used to analyse the relationship between the heat content anomalies in the warm pool (WP) area of the western Pacific and onset of South China Sea summer monsoon (SCSM).
利用1955～1998年逐月的上层海洋热含量资料和NCEP/NCAR再分析资料,研究了南海夏季风爆发与热带西太平洋暖池区热含量异常的关系,并对影响过程进行了探讨。
5) southwest monsoon
西南季风
1.
A preliminary analysis on the distribution characteristics of the air-sea latent heat flux over the SCS and its impact on the onset of southwest monsoon;
南海海气界面潜热通量的分布特征及其对西南季风爆发影响的初步分析
2.
The response of Holocene extreme floods in the Upper Changjiang River to changes of southwest monsoon
长江上游全新世特大洪水对西南季风变化的响应
3.
The analysis results show that Bilis was affected by the southwest monsoon and got a lot of vapor and energy supplies,while Kaemi did not have such supplies,so precipitation in the south of Kaemi is smaller than that of Bilis.
分析结果表明,"碧利斯"与"格美"前期都没有与北方冷空气发生作用,后期前者受到西南季风槽的影响得到大量水汽能量补充,在台风路径左侧产生强降水,后者的水汽、动力和能量条件较差,在华南产生的降水相对弱一些,但在北方冷空气的影响下在黄河中下游部分地区造成洪涝灾害。
6) 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。
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