Research Article
Synergy Effects of the Indian Summer Monsoon and the Tibetan Plateau Heating on Summer Rainfall over North China
Figure 8
Steady 500 hPa height (contours, units: gpm) and 500 hPa wind (vectors, units: m·s−1) anomalies generated by COM on (a) day 1, (b) day 5, (c) day 10, and (d) day 15.
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