Research Article
Analysis of a Late-Autumn Rainstorm in the Sichuan Basin on the Eastern Side of the Tibetan Plateau
Figure 13
The θse profile line distribution at (106°E 30°N) (K) (a); the CAPE (solid line, J·kg−1), and CIN (dashed line, J·kg−1) (b); the vertical velocity (Pa·s−1) (c); and the vorticity (solid line) and divergence (shading) (10−5 s−1) (d).
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