Research Article
Synergy Effects of the Indian Summer Monsoon and the Tibetan Plateau Heating on Summer Rainfall over North China
Figure 11
The linear regression pattern of the quasi-geostrophic stream function anomaly (QG) (contours, units: 106 m2·s−1) and T-N wave activity flux (TNF) (vectors, units: m2·s−2) at 200 hPa against (a) NCR, (b) INR, and (c) ISR. Dark (light) shadings indicate values significantly exceeding the 99% (90%) confidence level using Student’s t test.
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