Arid Land Geography ›› 2021, Vol. 44 ›› Issue (5): 1365-1372.doi: 10.12118/j.issn.1000–6060.2021.05.17
• Earth Surface Process • Previous Articles Next Articles
CHEN Shuo1,2(),DUAN Weili1,2(),LI Xiaoyang1,2
Received:
2020-11-16
Revised:
2021-05-09
Online:
2021-09-25
Published:
2021-09-22
Contact:
Weili DUAN
E-mail:chenshuo18@mails.ucas.ac.cn;duanweili@ms.xjb.ac.cn
CHEN Shuo,DUAN Weili,LI Xiaoyang. Runoff changes of the Aksu River under different exploitation scenarios in the upper river[J].Arid Land Geography, 2021, 44(5): 1365-1372.
Tab. 4
Interdecadal variation of runoff in Sary-Jaz River from 1958 to 2015"
时段 | 平均径流 /108 m3 | 距平 百分比/% | 丰枯 判别 | 径流最大年 | 径流最小年 | |||
---|---|---|---|---|---|---|---|---|
径流量/108 m3 | 年份 | 径流量/108 m3 | 年份 | |||||
1958—1959年 | 41.59 | -14 | 偏枯水 | 46.35 | 1959 | 36.84 | 1958 | |
1960—1969年 | 45.47 | -6 | 平水 | 53.08 | 1961 | 39.97 | 1964 | |
1970—1979年 | 43.96 | -9 | 平水 | 62.24 | 1978 | 36.37 | 1972 | |
1980—1989年 | 47.52 | -2 | 平水 | 51.95 | 1984 | 42.38 | 1989 | |
1990—1999年 | 54.56 | 13 | 偏丰水 | 69.96 | 1997 | 41.83 | 1993 | |
2000—2009年 | 52.46 | 8 | 平水 | 64.07 | 2002 | 36.98 | 2009 | |
2010—2015年 | 47.61 | -2 | 平水 | 55.38 | 2010 | 37.87 | 2014 | |
多年平均径流 | 48.42 | — | — | — | — | — | — |
Tab. 5
Multiple linear regression equations of the runoff in Sary-Jaz, Aksai and Aksu Rivers"
尺度 | 方程 | R2 | F值 | P值 |
---|---|---|---|---|
春季 | Y=0.386+0.368X1+0.882X2 | 0.591 | 39.676 | 0.000 |
夏季 | Y=-6.575+0.675X1+0.990X2 | 0.779 | 97.106 | 0.000 |
秋季 | Y=1.004+0.897X1+0.853X2 | 0.654 | 51.882 | 0.000 |
冬季 | Y=8.274-1.418X1+0.222X2 | 0.192 | 6.538 | 0.003 |
年 | Y=-2.549+0.783X1+0.897X2 | 0.778 | 96.499 | 0.000 |
Tab. 6
Sensitivity analysis of runoff in lower Aksu River on annual and seasonal scale to the Sary-Jaz River runoff reduction"
萨雷扎兹河入境水量 减少量/% | 阿克苏河下游径流量变化/% | ||||
---|---|---|---|---|---|
春季 | 夏季 | 秋季 | 冬季 | 年 | |
10 | -6.25 | -8.81 | -5.75 | -0.77 | -6.89 |
15 | -9.35 | -13.20 | -8.65 | -1.16 | -10.35 |
20 | -12.44 | -17.59 | -11.54 | -1.56 | -13.81 |
25 | -15.54 | -21.97 | -14.44 | -1.95 | -17.26 |
30 | -18.64 | -26.36 | -17.34 | -2.34 | -20.72 |
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