Analysis of a Late-Autumn Rainstorm in the Sichuan Basin on the Eastern Side of the Tibetan Plateau

Figure 13

The θ_se 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).

(a)

(b)

(c)

(d)