Research Article
Observational and Simulative Study of a Local Severe Precipitation Event Caused by a Cold Vortex over Northeast China
Figure 3
Geopotential height (black solid contours, gpm) and temperature (red dashed contours, °C) at 500 hPa and relative humidity (shaded, %) and wind vectors (m s−1) at 850 hPa. X1 and X2 are the same as in Figure 1: (a) 12:00 on the 27th, (b) 18:00 on the 27th, and (c) 00:00 on the 28th.
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