Research Article
Research on Historical and Future Spatial-Temporal Variability of Precipitation in China
Table 5
Decadal change of stable area and active area of each type of zone simulated by different climate models.
| Class | Time | M1 | M2 | M3 | M4 | M5 | Mean | S | A | S | A | S | A | S | A | S | A | S | A |
| I | 2010s | 18.3 | 13.7 | 21.8 | 8.3 | 21.9 | 9.6 | 21.3 | 6.5 | 21.1 | 13.1 | 20.9 | 10.2 | 2020s | 20.0 | 12.9 | 20.9 | 9.9 | 20.5 | 11.8 | 21.5 | 7.9 | 22.0 | 9.4 | 21.0 | 10.4 | 2030s | 18.4 | 13.8 | 21.8 | 11.1 | 20.4 | 12.0 | 20.6 | 7.8 | 20.7 | 9.7 | 20.4 | 10.9 | 2040s | 19.3 | 13.1 | 21.4 | 9.4 | 21.2 | 8.7 | 20.1 | 7.1 | 21.6 | 10.6 | 20.7 | 9.8 |
| II | 2010s | 3.1 | 35.3 | 6.1 | 27.2 | 3.9 | 26.0 | 6.6 | 24.2 | 2.8 | 30.7 | 28.7 | 4.5 | 2020s | 3.8 | 31.3 | 3.7 | 31.0 | 3.7 | 30.9 | 4.8 | 24.3 | 6.1 | 27.5 | 29.0 | 4.4 | 2030s | 2.9 | 34.9 | 4.8 | 29.8 | 3.2 | 28.8 | 4.8 | 28.9 | 5.7 | 27.7 | 30.0 | 4.3 | 2040s | 2.6 | 30.4 | 5.5 | 29.4 | 3.6 | 22.5 | 4.8 | 22.9 | 2.9 | 28.0 | 26.6 | 3.9 |
| III | 2010s | 9.5 | 38.2 | 9.6 | 31.5 | 12.4 | 33.5 | 10.4 | 32.8 | 9.0 | 31.7 | 10.2 | 33.5 | 2020s | 12.3 | 32.6 | 6.9 | 36.4 | 6.9 | 36.8 | 12.8 | 39.0 | 7.9 | 30.7 | 9.4 | 35.1 | 2030s | 9.8 | 39.3 | 5.9 | 34.3 | 8.2 | 39.7 | 10.3 | 34.8 | 9.6 | 31.5 | 8.7 | 35.9 | 2040s | 8.8 | 37.3 | 8.1 | 32.6 | 14.1 | 31.4 | 13.8 | 29.6 | 13.3 | 27.8 | 11.6 | 31.7 |
| IV | 2010s | 18.1 | 18.6 | 22.8 | 14.2 | 19.6 | 16.9 | 22.4 | 15.7 | 22.8 | 15.4 | 21.1 | 16.2 | 2020s | 19.3 | 13.5 | 23.3 | 17.9 | 22.1 | 17.5 | 14.1 | 22.8 | 24.4 | 12.7 | 20.6 | 16.9 | 2030s | 17.8 | 18.0 | 23.4 | 17.9 | 18.7 | 22.4 | 22.3 | 16.6 | 23.2 | 15.1 | 21.1 | 18.0 | 2040s | 21.0 | 19.7 | 23.8 | 14.1 | 21.8 | 17.6 | 24.7 | 13.7 | 24.7 | 9.7 | 23.2 | 15.0 |
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M1~M5 represent GFDL-ESM2M, HadGEM2-ES, IPSL-CM5A-LR, MIROC-ESM-CHEM, and NorESM1-M, respectively.
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