Articles | Volume 5, issue 2
https://doi.org/10.5194/esd-5-441-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esd-5-441-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Contrasting roles of interception and transpiration in the hydrological cycle – Part 1: Temporal characteristics over land
Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, the Netherlands
Stockholm Resilience Centre, Stockholm University, Stockholm, Sweden
R. J. van der Ent
Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, the Netherlands
L. J. Gordon
Stockholm Resilience Centre, Stockholm University, Stockholm, Sweden
H. H. G. Savenije
Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, the Netherlands
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Latest update: 13 Dec 2024
Short summary
We investigate the temporal characteristics of partitioned evaporation on land, and we present STEAM (Simple Terrestrial Evaporation to Atmosphere Model) -- a hydrological land-surface model developed to provide inputs to moisture tracking. The terrestrial residence timescale of transpiration (days to months) has larger inter-seasonal variation and is substantially longer than that of interception (hours). This can cause differences in moisture recycling, which is investigated more in Part 2.
We investigate the temporal characteristics of partitioned evaporation on land, and we present...
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