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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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The relationship between controlling parameters of annual catchment water balance and climate seasonality (S) and vegetation coverage (M) was discussed under the Budyko framework and an empirical equation was further developed so that the contributions from M to actual evapotranspiration (ET) could be determined more accurately. The results showed that the effects of landscape condition changes to ET variation will be estimated with a large error if the impacts of S are ignored.
Articles | Volume 21, issue 3
Hydrol. Earth Syst. Sci., 21, 1515–1526, 2017
https://doi.org/10.5194/hess-21-1515-2017

Special issue: Modeling hydrological processes and changes

Hydrol. Earth Syst. Sci., 21, 1515–1526, 2017
https://doi.org/10.5194/hess-21-1515-2017

Research article 10 Mar 2017

Research article | 10 Mar 2017

Vegetation dynamics and climate seasonality jointly control the interannual catchment water balance in the Loess Plateau under the Budyko framework

Tingting Ning et al.

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Cited articles

Berghuijs, W. R. and Woods, R. A.: Correspondence: Space-time asymmetry undermines water yield assessment, Nature Communications, 7, 11603, https://doi.org/10.1038/ncomms11603, 2016.
Budyko, M. I.: Evaporation under natural conditions, Gidrometeorizdat, Leningrad, English translation by IPST, Jerusalem, 1948.
Budyko, M. I. and Zubenok, L. I.: Determination of evaporation from the land surface, Izv. Akad.Nauk SSR, Ser. Geogr., 6, 3–17, 1961 (in Russian).
Budyko, M. I.: Climate and life, Academic, New York, 1974.
Carmona, A. M., Sivapalan, M., Yaeger, M. A., and Poveda, G.: Regional patterns of interannual variability of catchment water balances across the continental US: A Budyko framework, Water Resour. Res., 50, 9177–9193, https://doi.org/10.1002/2014wr016013, 2014.
Publications Copernicus
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Short summary
The relationship between controlling parameters of annual catchment water balance and climate seasonality (S) and vegetation coverage (M) was discussed under the Budyko framework and an empirical equation was further developed so that the contributions from M to actual evapotranspiration (ET) could be determined more accurately. The results showed that the effects of landscape condition changes to ET variation will be estimated with a large error if the impacts of S are ignored.
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