Journal cover Journal topic
Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
Hydrol. Earth Syst. Sci., 18, 4635-4655, 2014
http://www.hydrol-earth-syst-sci.net/18/4635/2014/
doi:10.5194/hess-18-4635-2014
© Author(s) 2014. This work is distributed
under the Creative Commons Attribution 3.0 License.
Opinion article
26 Nov 2014
HESS Opinions: From response units to functional units: a thermodynamic reinterpretation of the HRU concept to link spatial organization and functioning of intermediate scale catchments
E. Zehe1, U. Ehret1, L. Pfister2, T. Blume3, B. Schröder4,5, M. Westhoff1, C. Jackisch1, S. J. Schymanski6, M. Weiler7, K. Schulz8, N. Allroggen9, J. Tronicke9, L. van Schaik4, P. Dietrich10, U. Scherer1, J. Eccard5,9, V. Wulfmeyer11, and A. Kleidon12 1Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany
2Centre de Recherche Public – Gabriel Lippmann, Belvaux, Luxembourg
3GFZ German Research Centre for Geosciences, Potsdam, Germany
4Technische Universität Braunschweig, Braunschweig, Germany
5Berlin-Brandenburg Institute of Advanced Biodiversity Research (BBIB), Berlin, Germany
6Swiss Federal Institute of Technology, Zurich, Switzerland
7University of Freiburg, Freiburg, Germany
8University of Natural Resources and Life Sciences, Vienna, Austria
9University of Potsdam, Potsdam, Germany
10Helmholtz Centre of Environmental Research, Leipzig, Germany
11Universität Hohenheim, Hohenheim, Germany
12Max Planck Institute for Biogeochemistry, Jena, Germany
Abstract. According to Dooge (1986) intermediate-scale catchments are systems of organized complexity, being too organized and yet too small to be characterized on a statistical/conceptual basis, but too large and too heterogeneous to be characterized in a deterministic manner. A key requirement for building structurally adequate models precisely for this intermediate scale is a better understanding of how different forms of spatial organization affect storage and release of water and energy. Here, we propose that a combination of the concept of hydrological response units (HRUs) and thermodynamics offers several helpful and partly novel perspectives for gaining this improved understanding. Our key idea is to define functional similarity based on similarity of the terrestrial controls of gradients and resistance terms controlling the land surface energy balance, rainfall runoff transformation, and groundwater storage and release. This might imply that functional similarity with respect to these specific forms of water release emerges at different scales, namely the small field scale, the hillslope, and the catchment scale. We thus propose three different types of "functional units" – specialized HRUs, so to speak – which behave similarly with respect to one specific form of water release and with a characteristic extent equal to one of those three scale levels. We furthermore discuss an experimental strategy based on exemplary learning and replicate experiments to identify and delineate these functional units, and as a promising strategy for characterizing the interplay and organization of water and energy fluxes across scales. We believe the thermodynamic perspective to be well suited to unmask equifinality as inherent in the equations governing water, momentum, and energy fluxes: this is because several combinations of gradients and resistance terms yield the same mass or energy flux and the terrestrial controls of gradients and resistance terms are largely independent. We propose that structurally adequate models at this scale should consequently disentangle driving gradients and resistance terms, because this optionally allows equifinality to be partly reduced by including available observations, e.g., on driving gradients. Most importantly, the thermodynamic perspective yields an energy-centered perspective on rainfall-runoff transformation and evapotranspiration, including fundamental limits for energy fluxes associated with these processes. This might additionally reduce equifinality and opens up opportunities for testing thermodynamic optimality principles within independent predictions of rainfall-runoff or land surface energy exchange. This is pivotal to finding out whether or not spatial organization in catchments is in accordance with a fundamental organizing principle.

Citation: Zehe, E., Ehret, U., Pfister, L., Blume, T., Schröder, B., Westhoff, M., Jackisch, C., Schymanski, S. J., Weiler, M., Schulz, K., Allroggen, N., Tronicke, J., van Schaik, L., Dietrich, P., Scherer, U., Eccard, J., Wulfmeyer, V., and Kleidon, A.: HESS Opinions: From response units to functional units: a thermodynamic reinterpretation of the HRU concept to link spatial organization and functioning of intermediate scale catchments, Hydrol. Earth Syst. Sci., 18, 4635-4655, doi:10.5194/hess-18-4635-2014, 2014.
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