Stable water isotope tracing through hydrological models for disentangling runoff generation processes at the hillslope scale

Hillslopes are the dominant landscape components where incoming precipitation becomes groundwater, streamflow or atmospheric water vapor. However, directly observing flux partitioning in the soil is almost impossible. Hydrological hillslope models are therefore being used to investigate the processe...

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Bibliographic Details
Main Authors: D. Windhorst, P. Kraft, E. Timbe, H.-G. Frede, L. Breuer
Format: Article
Language:English
Published: Copernicus Publications 2014-10-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/18/4113/2014/hess-18-4113-2014.pdf