Research Article
Synergy Effects of the Indian Summer Monsoon and the Tibetan Plateau Heating on Summer Rainfall over North China
Figure 7
(a) Steady 200 hPa height anomalies (contours, unit: gpm), (b) 500 hPa height (contours, unit: gpm) and winds (vectors, unit: m·s−1) anomalies, and (c) 850 hPa winds anomalies (vectors, unit: m·s−1) generated by INH experiment, (d)–(f) is as (a)–(c), but for TPC experiment.
| (a) |
| (b) |
| (c) |
| (d) |
| (e) |
| (f) |