东北冷涡背景下两次强降水干侵入特征对比分析 |
段云霞, 崔锦, 李得勤, 王月, 班伟龙, 刘青 |
Comparative analysis of the characteristics of dry intrusions during two heavy rainfall processes under Northeast Cold Vortex background |
DUAN Yunxia, CUI Jin, LI Deqin, WANG Yue, BAN Weilong, LIU Qing |
图2 2016年 6月30日(a、b)与 2020年8月3日(c、d)08:00(a、c)和20:00(b、d)500 hPa高度场(黑色等值线,单位:gpm)、850 hPa风场(风矢,单位:m·s-1)、温度场(红色等值线,单位:℃)及相对湿度场(填色,单位:%) (红色三角形为沈阳所在位置) |
Fig.2 The 500 hPa geopotential height field (black isolines, Unit: gpm), 850 hPa wind field (wind vectors, Unit: m·s-1), temperature field (red isolines, Unit: ℃) and relative humidity (the color shaded, Unit: %) at 08:00 (a, c) and 20:00 (b, d ) on June 30, 2016 (a, b) and August 3, 2020 (c, d) (The red triangle is the position of Shenyang) |
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