一次典型东风波极端暴雨的中尺度特征及地形影响分析
Analysis of mechanism of topographic influence and meso-scale convective characteristics of an extremely severe rainfall affected by typical easterly wave
一次典型东风波极端暴雨的中尺度特征及地形影响分析 |
| 胡振菊, 黎璐, 黄小玉, 何炳文, 叶日新 |
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Analysis of mechanism of topographic influence and meso-scale convective characteristics of an extremely severe rainfall affected by typical easterly wave |
| HU Zhenju, LI Lu, HUANG Xiaoyu, HE Binwen, YE Rixin |
| 图8 2016年8月10日20:00(a、c、d)、11日02:00(b)850 hPa风场(箭矢,单位:m·s-1)和水汽通量散度(阴影,单位:10-5 g·hPa-1·cm-2·s-1)(a、b),850 hPa风场(箭矢,单位:m·s-1)和假相当位温θse(阴影,单位:K)(c), 500 hPa风场(箭矢,单位:m·s-1)及Δθse850-500(阴影,单位:K)(d) |
| Fig.8 The wind field (the vectors, Unit: m·s-1) and water vapor flux divergence (the shaded, Unit: 10-5 g·hPa-1·cm-2·s-1) on 850 hPa (a, b), the wind field (the vectors, Unit: m·s-1) and θse (the shaded, Unit: K) on 850 hPa (c), the wind field (the vectors, Unit: m·s-1) on 500 hPa and Δθse850-500 (the shaded, Unit: K) (d) at 20:00 BST 10 (a, c, d) and 02:00 BST 11 (b) August 2016 |
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