台风“罗莎”影响东北冷涡强降水的机理研究
李明珊, 王元兵, 王元

Influence of typhoon "Rosa" on the heavy rainfall of Northeast China cold vortex
Mingshan Li, Yuanbing Wang, Yuan Wang
图5 6 h模拟累积降水量(阴影,单位:mm·(6 h)-1) (a) 15日00时至15日06时,(b) 16日06时至16日12时,(c) 17日00时至17日06时,以及过强降水中心的位温(等值线,单位:K)及相对湿度(阴影,%)垂直剖面图(d) 15日03时,
(e) 16日09时,(f) 17日03时(剖面见图5a~c红色线)
Fig.5 WRF simulated 6 h accumulative?precipitation (shaded,unit:mm·(6 h)-1) in the (a) from 00:00 to 06:00 on the 15th,(b) from 06:00 to 12:00 on the 16th,(c) from 00:00 to 06:00 on the 17th,vertical cross?sections of the potential temperature (contour,unit:K) and relative humidity (shaded,%) along the rainstorms center at (d) 03:00 on the 15th,
(e) 09:00 on the 16th,and (f) 03:00 on the 17th,the red line in Fig.5a~c are the section lines