一次导致大风的暖区飑线后侧入流分析
桑明慧, 竹利, 沈晓玲, 张春艳, 左骏

Analysis about the rear inflow of a warm zone squall line causing strong winds
SANG Minghui, ZHU Li, SHEN Xiaoling, ZHANG Chunyan, ZUO Jun
图4 2018年3月4日17:30(a)、18:00(b)、18:30(c)、19:00(d)模拟的最大反射率因子(填色,单位:dBZ)及0~6 km(等值线)与0~3 km(矢量)垂直风切变(单位:m·s-1)分布
AB为飑线移动方向)
Fig.4 The distribution of simulated maximum reflectivity factor(the color shaded,Unit: dBZ),0-6 km(isolines) and 0-3 km(vectors) vertical wind shear(Unit: m·s-1) at 17:30(a),18:00(b),18:30(c) and 19:00(d) on 4 March 2018
(The AB is moving direction of the squall line)