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      Water Flux Tracking With a Distributed Hydrological Model to Quantify Controls on the Spatiotemporal Variability of Transit Time Distributions

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          A physically based, variable contributing area model of basin hydrology / Un modèle à base physique de zone d'appel variable de l'hydrologie du bassin versant

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            A Closed-form Equation for Predicting the Hydraulic Conductivity of Unsaturated Soils1

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              The prediction of hillslope flow paths for distributed hydrological modelling using digital terrain models

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                Author and article information

                Contributors
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                Journal
                Water Resources Research
                Water Resour. Res.
                Wiley
                00431397
                April 2018
                April 2018
                April 24 2018
                : 54
                : 4
                : 3081-3099
                Affiliations
                [1 ]Institute of Environmental Engineering, ETH Zurich; Zurich Switzerland
                [2 ]Department of Environmental Systems Science; ETH Zurich; Zurich Switzerland
                [3 ]Swiss Federal Research Institute WSL; Birmensdorf Switzerland
                [4 ]Department of Earth and Planetary Science; University of California; Berkeley CA USA
                Article
                10.1002/2017WR021689
                ca0ed71d-ae5f-4a58-82fc-8da4d8e7c3ca
                © 2018

                http://doi.wiley.com/10.1002/tdm_license_1.1

                http://onlinelibrary.wiley.com/termsAndConditions#vor

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