1) Condensation heating over the BOB
孟加拉湾季风潜热加热
3) BOB monsoon
孟加拉湾季风
1.
The physical linking between the BOB monsoon onset and SCS monsoon onset as well as the impacts of convective condensation heating associated with the BOB monsoon onset on the withdrawal of low level subtropical anticyclone is investigated.
利用南海季风试验分析场和NCAR向外长波辐射通量(OLR)资料研究了1998年孟加拉湾季风和南海季风爆发期间副热带环流的大尺度和天气尺度特征,探讨了孟加拉湾季风爆发与南海季风爆发之间的物理联系及孟加拉湾季风气旋的对流凝结潜热释放对副热带高压“撤出”南海的影响。
4) heat source over the Bay of Bengal
孟加拉湾热源
1.
the responses of the Asian monsoon circulation to the annual anomaly of the heat source over the Bay of Bengal in summer and the annual relationship between the heat source and the precipitation of China in summer are analyzed .
当孟加拉湾热源异常强 (弱 )时,南亚高压偏西 (东 ),西太平洋副热带高压位置偏东(西);印度夏季风偏强 (弱),东亚热带季风偏弱 (强 )。
5) Bengal storm
孟加拉湾风暴
1.
The Bengal storm occurred during the 18~(th) and 19~(th) of May 2004 is simulated by a mesoscale numerical model MM5V3.
利用MM5V3中尺度数值预报模式对2004年5月18~19日造成云南暴雨过程的孟湾风暴进行了数值模拟,在模拟结果与实况较为一致的基础上,利用辐散风和旋转风动能平衡方程,分析孟湾风暴的能量收支和转换特征,揭示孟加拉湾风暴维持的机制及其与外围暴雨增幅的关系。
2.
The NCEP-NCAR data is used to analyze the structures of the Bengal storm landing on 29 April 2006,before and after the landfalling,by means of the WRF(Weather Research and Forecast) meso-scale numerical model.
采用NCEP-NCAR再分析资料,分析了2006年4月29日登陆缅甸并造成云南省强降水过程的孟加拉湾风暴结构。
6) Bengal Bay
孟加拉湾
1.
Evolution and Eastward Movement Characteristics of Convective Cloud Clusters over Bengal Bay during Heavy Rains in Guangxi;
广西大范围暴雨期间孟加拉湾强对流演变及东移特征
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