风廓线雷达资料在一次对流暴雨过程中的特征分析 |
王文波, 李晓利, 曹云飞, 杨明, 高晓梅, 杨萌 |
Characteristic analysis of wind profile radar data in a convective rainstorm |
WANG Wenbo, LI Xiaoli, CAO Yunfei, YANG Ming, GAO Xiaomei, YANG Meng |
图5 2023年6月27日03:30 100 m(a)、300 m(b)、900 m(c)、1 500 m(d)、3 000 m(e)、6 000 m(f)散度(等值线,单位:10-5 s-1)、涡度平流(填色,单位:10-9 s-2)及风场(风向杆,单位:m·s-1) (黑色三角为风廓线雷达站点,下同) |
Fig.5 The divergence (the contour lines, Unit: 10-5 s-1), vorticity advection (the color shaded, Unit: 10-9 s-2) and wind field (wind direction poles, Unit: m·s-1) at 100 m (a), 300 m (b), 900 m (c), 1 500 m (d), 3 000 m (e), and 6 000 m (f) at 03:30 on 27 June, 2023 (The black triangle indicates wind profile radar station, the same as below) |
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