Attributing Urban Evapotranspiration From Eddy‐Covariance to Surface Cover: Bottom‐Up Versus Top‐Down

Attributing Urban Evapotranspiration From Eddy‐Covariance to Surface Cover: Bottom‐Up Versus Top‐Down

Abstract Evapotranspiration (ET) is a key process in the hydrological cycle that can help mitigate urban heat. ET depends on the surface cover, as the surface affects the partitioning of precipitation between runoff and evapotranspiration. In urban neighborhoods, this surface cover is highly heterog...

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Bibliographic Details
Main Authors: H. J. Jongen, S. Vulova, F. Meier, G. J. Steeneveld, F. A. Jansen, D. Tetzlaff, B. Kleinschmit, N. Haacke, A. J. Teuling
Format: Article
Language:English
Published: Wiley 2024-09-01
Series:Water Resources Research
Subjects:
urban climate
footprint modeling
evaporation
eddy‐covariance observations
surface cover
urban hydrology
Online Access:https://doi.org/10.1029/2024WR037508
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