Orographic Effect and the Opposite Trend of Rainfall in Central Vietnam

<div>OLR (<i>shaded</i>, Wm<sup>−2</sup>), 850 hPa wind (<i>vector</i>, ms<sup>−1</sup>) and geopotential height (<i>contour</i>, m) anomalies regressed on the PC1 (a) and PC2 (b). (a) OLR,wind, hgt regreseed on PC1. (b) OLR,wind, hgt regressed on PC2.</div>

Advances in Meteorology

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Figure 8

Figure 8: Orographic Effect and the Opposite Trend of Rainfall in Central Vietnam 