西北干旱区一次极端暴雨局地性增强的对流环境特征
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傅朝( ), 刘维成( ), 宋兴宇, 徐丽丽, 沙宏娥, 马莉, 崔宇
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Local enhanced convective environment characteristics of an extreme rainstorm event in arid region of Northwest China
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FU Zhao( ), LIU Weicheng( ), SONG Xingyu, XU Lili, SHA Honge, MA Li, CUI Yu
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图6. 2022年8月12日20:00(a、c)和13日00:00(b、d)金塔站T-ln P图(a、b)和对流有效位能(CAPE)(单位:J·kg-1)(c、d) (红实线为层结曲线,黑实线为状态曲线,绿实线为露点温度线)
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Fig.6. T-ln P diagram (a, b) at Jinta station and convective effective potential energy (CAPE) (Unit: J·kg-1) (c, d) at 20:00 BST 12 August (a, c) and 00:00 BST on 13 August (b, d) 2022 (The red, black, green solid lines are stratification curve, state curve and dew point temperature, respectively)
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