Articles | Volume 20, issue 1
https://doi.org/10.5194/hess-20-479-2016
https://doi.org/10.5194/hess-20-479-2016
Research article
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28 Jan 2016
Research article | Highlight paper |  | 28 Jan 2016

Does the Budyko curve reflect a maximum-power state of hydrological systems? A backward analysis

M. Westhoff, E. Zehe, P. Archambeau, and B. Dewals

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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (17 Oct 2015) by Dingbao Wang
AR by Martijn Westhoff on behalf of the Authors (06 Nov 2015)
ED: Referee Nomination & Report Request started (26 Nov 2015) by Dingbao Wang
RR by Anonymous Referee #1 (13 Dec 2015)
ED: Publish as is (11 Jan 2016) by Dingbao Wang
AR by Martijn Westhoff on behalf of the Authors (13 Jan 2016)
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Short summary
We derived mathematical formulations of relations between relative wetness and gradients driving run-off and evaporation for a one-box model such that, when conductances are optimized with the maximum power principle, the model leads exactly to a point on the Budyko curve. With dry spells and dynamics in actual evaporation added, the model compared well with catchment observations without calibrating any parameter. The maximum-power principle may thus be used to derive the Budyko curve.