An entropy-based measure of hydrologic complexity and its applications
Basin response and hydrologic fluxes are functions of hydrologic states, most notably of soil moisture. However, characterization of hillslope-scale soil moisture is challenging since it is both spatially heterogeneous and dynamic. This paper introduces an entropy-based and discretization-invariant...
| Main Authors: | , , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
American Geophysical Union
2017
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| Online Access: | http://hdl.handle.net/1721.1/110324 https://orcid.org/0000-0003-4265-1314 https://orcid.org/0000-0002-8362-4761 |