线状MCSs强降水特征及形成条件 |
许敏, 沈芳, 刘淇淇, 李娜, 王洁 |
Formation conditions and characteristics of heavy precipitation with quasi-linear MCSs |
XU Min, SHEN Fang, LIU Qiqi, LI Na, WANG Jie |
图1 典型3类线状MCSs强降水发生时北京雷达站1.5°仰角反射率因子(单位:dBZ) (a)2015年8月7日(TS型)19:18,(b)2012年7月25日(LS型)22:54,(c)2018年8月8日(PS型)10:06 |
Fig.1 Radar reflectivity factor at 1.5°elevation angle from Beijing radar station when the heavy precipitation with quasi-linear MCSs occurred (Unit: dBZ) (a) 19:18 BST on August 7,2015 (trailing stratiform type), (b) 22:54 BST June 25,2012 (leading stratiform type), (c) 10:06 BST August 8,2018 (parallel stratiform type) |
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