Research Article
Spatiotemporal Changes in Extreme Precipitation and Its Dependence on Topography over the Poyang Lake Basin, China
Table 5
Number and percentage of stations showing upward and downward trends for each extreme precipitation index.
| Index | Upward trend | Downward trend | Not sig. | Sig. at 0.1 | Total | Not sig. | Sig. at 0.1 | Total |
| EPD | 59 (78.7%) | 7 (9.3%) | 66 (88.0%) | 9 (12.0%) | 0 (0) | 9 (12.0%) | EPA | 63 (84.0%) | 5 (6.7%) | 68 (90.7%) | 7 (9.3%) | 0 (0) | 7 (9.3%) | EPI | 47 (62.7%) | 9 (12.0%) | 56 (74.7%) | 19 (25.3%) | 0 (0) | 19 (25.3%) | EPR | 45 (60.0%) | 24 (32.0%) | 69 (92.0%) | 6 (8.0%) | 0 (0) | 6 (8.0%) | CDD | 30 (40.0%) | 0 (0) | 30 (40.0%) | 40 (53.3%) | 5 (6.7%) | 45 (60.0%) | CWD | 16 (21.3%) | 0 (0) | 16 (21.3%) | 56 (74.7%) | 3 (4.0%) | 59 (78.7%) | Rx1d | 37 (49.3%) | 11 (14.7%) | 48 (64.0%) | 26 (34.7%) | 1 (1.3%) | 27 (36.0%) | Rx5d | 50 (66.7%) | 0 (0) | 50 (66.7%) | 25 (33.3%) | 0 (0) | 25 (33.3%) |
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