Table 4 The elasticity of streamflow alterations on climate variability and human activities.

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

Period

Budyko

Fu et al.

Choudhury

\({{\boldsymbol{\varepsilon }}}_{{\boldsymbol{P}}}\)

\({{\boldsymbol{\varepsilon }}}_{{\boldsymbol{E}}{{\boldsymbol{T}}}_{{\boldsymbol{P}}}}\)

\({{\boldsymbol{\varepsilon }}}_{{\boldsymbol{P}}}\)

\({{\boldsymbol{\varepsilon }}}_{{\boldsymbol{E}}{{\boldsymbol{T}}}_{{\boldsymbol{P}}}}\)

\({{\boldsymbol{\varepsilon }}}_{{\boldsymbol{m}}}\)

\({{\boldsymbol{\varepsilon }}}_{{\boldsymbol{P}}}\)

\({{\boldsymbol{\varepsilon }}}_{{\boldsymbol{E}}{{\boldsymbol{T}}}_{{\boldsymbol{P}}}}\)

\({{\boldsymbol{\varepsilon }}}_{{{\boldsymbol{n}}}_{{\bf{0}}}}\)

1960–1972

2.999

−1.999

1.044

−0.044

−0.501

1.061

−0.061

−0.791

1973–1986

2.998

−1.998

1.082

−0.082

−1.253

1.127

−0.127

−0.992

1987–2015

2.999

−1.999

1.128

−0.128

−1.975

1.261

−0.261

−1.884