Articles | Volume 17, issue 1
https://doi.org/10.5194/hess-17-225-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/hess-17-225-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Thermodynamics, maximum power, and the dynamics of preferential river flow structures at the continental scale
A. Kleidon
Max-Planck Institute for Biogeochemistry, Hans-Knöll-Str. 10, 07745 Jena, Germany
E. Zehe
Institute of Water Resources and River Basin Management, Karlsruhe Institute of Technology – KIT, Karlsruhe, Germany
Institute of Water Resources and River Basin Management, Karlsruhe Institute of Technology – KIT, Karlsruhe, Germany
U. Scherer
Institute of Water Resources and River Basin Management, Karlsruhe Institute of Technology – KIT, Karlsruhe, Germany
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- A topographic index explaining hydrological similarity by accounting for the joint controls of runoff formation R. Loritz et al. 10.5194/hess-23-3807-2019
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- Working at the limit: a review of thermodynamics and optimality of the Earth system A. Kleidon 10.5194/esd-14-861-2023
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- The hydrological system as a living organism H. Savenije 10.5194/piahs-385-1-2024
- Importance of temporal variability for hydrological predictions based on the maximum entropy production principle M. Westhoff et al. 10.1002/2013GL058533
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- Maximum energy dissipation to explain velocity fields in shallow reservoirs M. Westhoff et al. 10.1080/00221686.2017.1289268
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- Technical note: Inference in hydrology from entropy balance considerations S. Kollet 10.5194/hess-20-2801-2016
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