引发广西一次区域性暴雨的低涡发展机制 |
覃皓, 王志毅, 郭晓薇, 刘晓梅, 朱丽云 |
Development mechanisms of the vortex causing a regional rainstorm in Guangxi |
QIN Hao, WANG Zhiyi, GUO Xiaowei, LIU Xiaomei, ZHU Liyun |
图4 2022年6月10日08:00—11日08:00平均的850 hPa位势高度(等值线,单位:dagpm)、风场(箭矢,单位:m·s-1)和涡度平流项(填色,单位:10-8 s-1)(a)、垂直输送项(填色,单位:10-8 s-1)(b)、倾侧项(填色,单位:10-8 s-1)(c)、水平散度项(填色,单位:10-8 s-1)(d)分布 |
Fig.4 Distribution of geopotential height (contours, Unit: dagpm), wind (arrow vectors, Unit: m·s-1) and vorticity advection (the color shaded, Unit: 10-8 s-1) (a), vertical transfer (the color shaded, Unit: 10-8 s-1) (b), torsion (the color shaded Unit: 10-8 s-1) (c) and horizontal divergence (the color shaded, Unit: 10-8 s-1) (d) at 850 hPa averaged from 08:00 on 10 to 08:00 on 11 June 2022 |
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