Table 7 Peak and valley errors in test results for experiment 2.
From: An efficient parallel runoff forecasting model for capturing global and local feature information
Evaluation indicators | Sites | Sets | Model | |||||
|---|---|---|---|---|---|---|---|---|
PFN | Transformer | BiGRU | ||||||
Peak | Valley | Peak | Valley | Peak | Valley | |||
EP (%) | Dongjiang Station | 1 | 15.01 | 0.63 | 13.29 | 1.87 | 4.27 | 15.37 |
2 | 38.28 | 68.54 | 40.34 | 61.06 | 33.15 | 63.39 | ||
3 | 37.71 | 40.89 | 40.70 | 34.21 | 39.65 | 36.63 | ||
4 | 16.56 | 61.30 | 17.59 | 64.08 | 17.14 | 67.31 | ||
5 | 22.60 | 18.05 | 22.27 | 32.01 | 18.06 | 62.78 | ||
6 | 32.64 | 131.54 | 40.06 | 139.75 | 44.95 | 179.53 | ||
7 | 27.12 | 43.16 | 24.33 | 36.69 | 13.66 | 45.53 | ||
8 | 45.27 | 1.56 | 49.20 | 5.27 | 62.72 | 37.39 | ||
9 | 8.93 | 3.12 | 8.87 | 3.24 | 1.31 | 16.42 | ||
10 | 7.76 | 1.97 | 13.35 | 5.18 | 12.58 | 11.70 | ||
Quinebaug River | 1 | 21.99 | 11.53 | 9.67 | 47.27 | 25.71 | 11.92 | |
2 | 4.41 | 16.68 | 6.02 | 40.71 | 11.55 | 8.66 | ||
3 | 43.28 | 4.52 | 49.74 | 26.08 | 52.82 | 0.05 | ||
4 | 25.74 | 0.42 | 29.80 | 3.64 | 29.06 | 40.35 | ||
5 | 30.42 | 16.93 | 47.06 | 25.75 | 41.07 | 63.47 | ||
6 | 41.48 | 8.93 | 61.39 | 19.25 | 75.40 | 46.24 | ||
7 | 19.28 | 121.95 | 7.31 | 181.84 | 17.84 | 150.03 | ||
8 | 23.82 | 172.73 | 3.40 | 198.51 | 33.29 | 187.68 | ||
9 | 30.60 | 118.83 | 0.44 | 181.11 | 34.31 | 159.06 | ||
10 | 39.08 | 212.69 | 22.02 | 259.31 | 30.88 | 259.59 | ||
11 | 2.61 | 195.80 | 20.41 | 267.06 | 2.71 | 235.28 | ||
12 | 34.81 | 25.08 | 16.48 | 70.12 | 38.91 | 41.15 | ||
Housatonic River | 1 | 6.52 | 11.50 | 9.54 | 28.91 | 2.29 | 32.61 | |
2 | 3.96 | 5.93 | 10.21 | 17.05 | 8.34 | 28.72 | ||
3 | 13.69 | 3.14 | 2.34 | 14.91 | 33.71 | 22.94 | ||
4 | 15.66 | 6.95 | 23.12 | 9.22 | 39.55 | 30.29 | ||
5 | 23.48 | 6.79 | 27.89 | 33.40 | 38.93 | 31.90 | ||
6 | 16.73 | 6.73 | 14.53 | 54.39 | 34.13 | 40.55 | ||
7 | 17.41 | 20.40 | 6.15 | 109.48 | 12.86 | 75.02 | ||
8 | 19.54 | 19.86 | 33.41 | 130.34 | 10.92 | 99.32 | ||
9 | 66.12 | 21.89 | 52.86 | 131.48 | 52.08 | 100.90 | ||
10 | 30.48 | 5.64 | 3.62 | 77.30 | 14.05 | 50.18 | ||
11 | 15.63 | 2.29 | 18.90 | 60.17 | 17.40 | 38.00 | ||
12 | 2.33 | 6.42 | 2.43 | 74.00 | 23.89 | 44.64 | ||