Research Article
Synergy Effects of the Indian Summer Monsoon and the Tibetan Plateau Heating on Summer Rainfall over North China
Figure 4
(a) Regression maps of 850 hPa wind (vectors, units: m·s−1) anomalies against (a) NCR, (b) TPR, and (c) ISR for JA during 1979–2007. Dark (light) shadings indicate values significantly exceeding the 99% (90%) confidence level using Student’s t test.
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