登陆华东台风降水分布特征
郑林晔, 谌芸, 冯恬, 姚梦颖

Precipitation characteristics of typhoons landfall in East China
ZHENG Linye, CHEN Yun, FENG Tian, YAO Mengying
图8 L型(a、c、e)和R型(b、d、f)内核降水台风登陆时(a、b)和登陆后12 h(c、d)、24 h(e、f)1000 hPa涡度场(红色线,单位:10-5s-1)、200 hPa风场(矢量,单位:m·s-1)及850 hPa垂直速度(彩色填色区,单位:10-1 Pa·s-1)动态合成
(红色方框区域为高层辐散区)
Fig.8 The dynamic synthesis of vorticity field at 1000 hPa (red lines, Unit: 10-5s-1), wind field at 200 hPa (vectors, Unit: m·s-1) and vertical velocity at 850 hPa (color shaded areas, Unit: 10-1 Pa·s-1) at the time of landing (a, b)and 12 hours (c, d),24 hours (e, f) after the landing of L-type (a、c、e) and R-type (b、d、f) core precipitation typhoon
(The area in red box are high-level divergence area)