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7 2022年6月10—11日850 hPa绝对涡度(等值线,单位:10-5 s-1)、非地转风场(箭矢,单位:m·s-1)及其水平散度(填色,单位:10-5 s-1)分布 (红色实线框为低涡中心北侧,红色箭头代表实框中平均风向,红色虚线框为低涡中心) |
Fig.7 Distribution of absolute vorticity (isolines, Unit: 10-5 s-1), ageostrophic wind filed (arrow vectors, Unit: m·s-1) and its horizontal divergence (the color shaded, Unit: 10-5 s-1) at 850 hPa from 10 to 11 June 2022 (The red solid line box is the north side of the vortex center, the red arrow represents the average wind direction in the solid line box, the red dotted line box is the vortex center) |
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