How can we model subsurface stormflow at the catchment scale if we cannot measure it?-Reference-Cited by-同舟云学术

How can we model subsurface stormflow at the catchment scale if we cannot measure it?

Published:2019-02-21 Issue:9 Volume:33 Page:1378-1385
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Chifflard Peter¹^ORCID,Blume Theresa²,Maerker Katja³,Hopp Luisa⁴,Meerveld Ilja⁵,Graef Thomas⁶,Gronz Oliver⁷,Hartmann Andreas⁸,Kohl Bernhard⁹,Martini Edoardo¹⁰,Reinhardt‐Imjela Christian¹¹,Reiss Martin¹,Rinderer Michael⁸,Achleitner Stefan¹²

Affiliation:

1. Department of GeographyPhilipps‐University Marburg Marburg Germany

2. Department of HydrologyGerman Research Centre for Geosciences Potsdam Potsdam Germany

3. Department of Physical Geography(formerly Katja Heller) University of Technology Dresden Dresden Germany

4. Department of HydrologyUniversity of Bayreuth Bayreuth Germany

5. Department of Geography – Hydrology and ClimateUniversity of Zürich Zurich Switzerland

6. German Environment Agency Dessau‐Roßlau Germany

7. Department of Physical GeographyUniversity of Trier Trier Germany

8. Department of HydrologyAlbert‐Ludwigs‐University of Freiburg Freiburg im Breisgau Germany

9. Department of Natural HazardsAustrian Research Centre for Forests Innsbruck Innsbruck Austria

10. Institute of Environmental PhysicsRuprecht‐Karls‐University of Heidelberg Heidelberg Germany

11. Department of Applied Physical GeographyFreie Universitaet Berlin Berlin Germany

12. Unit for Hydraulic EngineeringUniversity of Innsbruck Innsbruck Austria

Funder

Deutsche Forschungsgemeinschaft

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.13407

Reference88 articles.

1. Comparison of threshold hydrologic response across northern catchments

2. Subsurface flow velocities in a hillslope with lateral preferential flow

3. Piezometric response in zones of a watershed with lateral preferential flow as a first-order control on subsurface flow

4. Form and function in hillslope hydrology: characterization of subsurface flow based on response observations

5. New Dimensions of Hillslope Hydrology

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