Research Article
Analysis of a Late-Autumn Rainstorm in the Sichuan Basin on the Eastern Side of the Tibetan Plateau
Figure 5
850 hPa wind field (m·s−1), 24-h temperature variation (shaded, °C), divergence value of less than −2 × 10−5 s−1 (color dashed line), and PEPT distribution (black solid line, °C) at (a) 1800 UTC 26 October 2014, (b) 0000 UTC 27 October 2014, (c) 1200 UTC 27 October 2014, and (d) 0000 UTC 28 October 2014. L—SWCV; J—LLJ. The thick solid line (black) and the curve with an arrow in (b)—inverted trough and its airflow direction; the thick solid line (red) in (d)—shear line; grey area—terrain of Tibetan Plateau.
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