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

Figure 4

Base reflectivity of Nanchong radar (dBZ) and corresponding 3 km height wind field of radar echo inversion (g and h) (m·s⁻¹) at (a–c, and g) 0105 UTC 27 October 2014, (d–f, and h) 1157 UTC 27 October 2014 (solid line—shear line; L—low vortex; solid-line arrows—small-scale LLJ) at the elevation of 0.5° (a, d), 1.5° (b, e), and 2.4° (c, f).

(a)

(b)

(c)

(d)

(e)

(f)

(g)

(h)