Research Article
Analysis of a Late-Autumn Rainstorm in the Sichuan Basin on the Eastern Side of the Tibetan Plateau
Figure 7
Cross section of vertical circulation along line A-A′ in Figure 6(a), in which the solid contours are the horizontal wind speed (“JU” is the ULJ axis), the shaded area is the vertical velocity (10−2 Pa·s−1), the stream line is the synthetic circulation of both horizontal wind (m·s−1) and vertical velocity (10−2 Pa·s−1), the thick solid lines with arrows are the airflow direction, and the black areas are the terrain, at (a) 0000 UTC 27 October 2014, (b) 0600 UTC 27 October 2014, (c) 1200 UTC 27 October 2014, and (d) 0000 UTC 28 October 2014.
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