京津冀地区一次极端暖区暴雨成因分析 |
| 董琪如, 王莹, 李英华, 杨旭, 梁康壮 |
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Causes analysis of an extreme warm-sector rainstorm in Beijing-Tianjin-Hebei region |
| DONG Qiru, WANG Ying, LI Yinghua, YANG Xu, LIANG Kangzhuang |
| 图9 2020年8月12日11:00(a)、13:00(b)、15:00(c)模拟的950 hPa水汽通量散度(填色,单位:10-6 g·cm-2·hPa-1·s-1)、风场(风矢,单位:m·s-1)、比湿(绿色等值线,单位:g·kg-1)、地形(线段填充区域,单位:m) (黑框为水汽强辐合区) |
| Fig.9 The simulated water vapour fux divergence (the color shaded,Unit: 10-6 g·cm-2·hPa-1·s-1),wind field (wind vectors,Unit: m·s-1),specific humidity (green isolines,Unit: g·kg-1) and terrain height (the area filled with line segments,Unit: m) at 950 hPa at 11:00 (a),13:00 (b),15:00 (c) on August 12,2020 (The black box denotes the region of intense water vapor convergence) |
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