Research Article
Synergy Effects of the Indian Summer Monsoon and the Tibetan Plateau Heating on Summer Rainfall over North China
Figure 6
The (a) in-depth mean of diabatic heating anomalies in 80°E, 22°N and cooling anomalies in 90°E, 30°N (units: K·day−1) and vertical profiles of forcing (units: K·day−1) in (b) 80°E, 22°N and (c) 90°E, 30°N used to drive the LBM model.
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