Table 3 Contributions of climate variability and human activities on streamflow alterations.

From: Identification of potential impacts of climate change and anthropogenic activities on streamflow alterations in the Tarim River Basin, China

Period

P(mm)

ETp(mm)

Q(mm)

m

n

\(\eta {1}_{clim}\)

\(\eta {1}_{hum}\)

\(\eta {2}_{clim}\)

\(\eta {2}_{hum}\)

\(\eta {3}_{clim}\)

\(\eta {3}_{hum}\)

\(\eta {4}_{clim}\)

\(\eta {4}_{hum}\)

1960–1972

38.7

2176.18

35.53

1.04

0.22

        

1973–1985

47.71

2084.82

30.22

1.08

0.28

−20.68%

120.68%

−22.06%

122.06%

−23.75%

123.75%

−44.60%

144.60%

1986–2011

53.87

1924.68

28.76

1.13

0.37

−90.14%

190.14%

−123.58%

223.58%

−128.68%

228.68%

−40.38%

140.38%

  1. Note: \(\eta {1}_{clim}\), \(\eta {2}_{clim}\), \(\eta {3}_{clim}\), \(\eta {4}_{clim}\) are the contribution rates of climate change in Budyko, Fu., Choudhury equations and DMC, respectively. \(\eta {1}_{hum}\), \(\eta {2}_{hum}\), \(\eta {3}_{hum}\), \(\eta {4}_{hum}\) are the contribution rates of human activities in Budyko, Fu., Choudhury equations and DMC, respectively.
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