Table 1 The time-lag based on the spatial correlations between the variables in the Historical and Hist-GHG simulations from pentads 25–40 over the region 20°–45°N, 105°–120°E (Unit: pentad)
From: Influence of aerosol forcing on the seasonal march of East Asia summer monsoon
Pentad | SSR | θse | T850 | T500 | q850 | V850 | V500 | WPSH* | He* | U200 | WJ* |
|---|---|---|---|---|---|---|---|---|---|---|---|
25 | −2 | −2 | −1 | −1 | −1 | 1 | −2 | −1 | 0 | −1 | 3 |
26 | −3 | −1 | −1 | 1 | −1 | −1 | −4 | 1 | −2 | 0 | 0 |
27 | −4 | −2 | −1 | 0 | −2 | −2 | −4 | 0 | −2 | −1 | 1 |
28 | −4 | −1 | 0 | 0 | 0 | −1 | 1 | 0 | 1 | 0 | 1 |
29 | −3 | −1 | −1 | 0 | 0 | 0 | −1 | 1 | 0 | 0 | 0 |
30 | −4 | 0 | −1 | −1 | 0 | −1 | −1 | 0 | 0 | 1 | −1 |
31 | −3 | −2 | −1 | 0 | −1 | −1 | −1 | −1 | −1 | 0 | 0 |
32 | 0 | 0 | −1 | 0 | 0 | 1 | 0 | 0 | −1 | 0 | 0 |
33 | −1 | −1 | −1 | −1 | −1 | 0 | −1 | 0 | −1 | −1 | 0 |
34 | −2 | −2 | −1 | −1 | −2 | −1 | −1 | 0 | −1 | −2 | −1 |
35 | 0 | −1 | −1 | −1 | −1 | 0 | 0 | 0 | 0 | −1 | −1 |
36 | −1 | −1 | −1 | −1 | 0 | 0 | 0 | 0 | 0 | −1 | −1 |
37 | 0 | −1 | −1 | 0 | −1 | 0 | 0 | 0 | 0 | 0 | 0 |
38 | 0 | −1 | −1 | −1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
39 | 0 | −1 | −2 | −1 | −1 | −2 | 0 | 0 | 0 | 0 | −1 |
40 | −1 | −2 | 3 | −1 | −1 | −1 | −1 | −1 | 2 | −1 | −1 |
41 | −2 | −2 | −1 | −1 | −2 | −1 | −1 | −1 | 1 | −1 | −1 |
42 | −3 | 2 | −1 | −2 | 2 | 1 | −1 | 0 | 1 | −1 | −1 |