The Unreasonable Effectiveness of the Budyko Hypothesis for Water Balance

Ross Woods, Wouter Berghuijs, Murugesu Sivapalan, H. H. G. Savenije

Research output: Contribution to conferenceConference Abstract

Abstract

The Budyko hypothesis, that the long-term evaporative fraction is primarily a function of the aridity index, is widely considered to be a hydrological success; perhaps this is because catchment hydrology has so few widely applicable constitutive equations!
The apparent success of the Budyko hypothesis seems paradoxical, given the complexity of hydrological processes, and the myriad of interacting factors which drive the partitioning of the water balance. For any given value of the aridity index, there is a very significant range in many factors that also affect water balance, including climate seasonality, rainfall intensity, landscape structure, soil type, vegetation cover and hydro-geological setting. In this talk we use a comparative hydrology approach with global, continental and regional datasets to explore two competing schools of thought: (i) the Budyko hypothesis is essentially correct, because climate, soil, vegetation and topography are strongly interdependent; (ii) the hypothesis is incomplete and requires extension to account for the significant effects on water balance of factors other than aridity.
Original languageEnglish
Publication statusPublished - 2013
EventFall Meeting of the American Geophysical Union - San Francisco, United States
Duration: 9 Dec 201313 Dec 2013

Conference

ConferenceFall Meeting of the American Geophysical Union
CountryUnited States
CitySan Francisco
Period9/12/1313/12/13

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  • Activities

    • 1 Invited talk

    Fall Meeting of the American Geophysical Union

    Ross Woods (Speaker)

    9 Dec 201313 Dec 2013

    Activity: Participating in or organising an event typesInvited talk

    Cite this

    Woods, R., Berghuijs, W., Sivapalan, M., & Savenije, H. H. G. (2013). The Unreasonable Effectiveness of the Budyko Hypothesis for Water Balance. Abstract from Fall Meeting of the American Geophysical Union, San Francisco, United States.