Articles | Volume 20, issue 6
Hydrol. Earth Syst. Sci., 20, 2195–2205, 2016
Hydrol. Earth Syst. Sci., 20, 2195–2205, 2016

Research article 08 Jun 2016

Research article | 08 Jun 2016

A two-parameter Budyko function to represent conditions under which evapotranspiration exceeds precipitation

Peter Greve et al.

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Cited articles

Adler, R. F., Huffman, G. J., Chang, A., Ferraro, R., Xie, P., Janowiak, J., Rudolf, B., Schneider, U., Curtis, S., Bolvin, D., Gruber, A., Susskind, J., Arkin, P., and Nelkin, E.: The version-2 global precipitation climatology project (GPCP) monthly precipitation analysis (1979–present), J. Hydrometeorol., 4, 1147–1167, 2003.
Berghuijs, W. R., Woods, R. A., and Hrachowitz, M.:A precipitation shift from snow towards rain leads to a decrease in streamflow, Nat. Clim. Change, 4, 583–586, 2014.
Budyko, M.: The Heat Balance of the Earth, Leningrad, 1956 (in Russian), Translation by N. A. Stepanova, US Weather Bureau, Washington, p. 255, 1958.
Budyko, M.: Climate and life, Academic Press, New York, USA, p. 508, 1974.
Chen, X., Alimohammadi, N., and Wang, D.: Modeling interannual variability of seasonal evaporation and storage change based on the extended Budyko framework, Water Resour. Res., 49, 6067–6078, 2013.
Short summary
The widely used Budyko framework is by definition limited to steady-state conditions. In this study we analytically derive a new, two-parameter formulation of the Budyko framework that represents conditions under which evapotranspiration exceeds precipitation. This is technically achieved by rotating the water supply limit within the Budyko space. The new formulation is shown to be capable to represent first-order seasonal dynamics within the hydroclimatological system.