ANN Model-Based Simulation of the Runoff Variation in Response to Climate Change on the Qinghai-Tibet Plateau, China
Table 10
The response of runoff to climate change at the Three-River Headwater Regions (m3/s).
Sites
Index
Normal
P10%
P20%
T0.5
T1.0
T2.0
T0.5
T1.0
T2.0
YARHR
Average runoff
416.51
471.16
498.16
561.68
478.58
505.57
567.11
Max
1277.95
1348.05
1374.07
1414.78
1353.04
1370.28
1422.16
Min
26.88
9.89
8.13
19.44
6.48
6.75
22.24
Average change
0
91.14
111.02
158.80
101.21
122.16
168.34
LARHR
Average runoff
460.30
457.03
453.29
445.67
472.54
468.90
461.48
Max
1098.51
1095.30
1093.81
1090.39
1097.25
1095.86
1092.67
Min
123.19
123.70
124.34
126.32
124.99
125.97
130.14
Average change
0
70.63
71.69
74.02
81.06
81.57
82.90
YERHR
Average runoff
566.75
568.95
565.84
559.67
575.08
572.04
566.01
Max
1192.67
1214.68
1210.26
1201.11
1239.65
1235.57
1227.12
Min
206.05
202.78
202.60
202.25
200.56
200.40
200.08
Average change
0
70.37
70.04
69.47
76.31
75.61
74.26
Note. (1) T0.5, T1.0, and T2.0 mean air temperature increased by 0.5°C, 1.0°C, and 2.0°C, respectively. P 10% and P 20% mean the precipitation increased by 10% and 20%, respectively.
