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  4. Evaporation dynamics from flowing water surfaces

Evaporation dynamics from flowing water surfaces

Citation Link: https://doi.org/10.15480/882.18703
Publikationstyp
Journal Article
Date Issued
2026-09-16
Sprache
German
Author(s)
Hou, Lintong
Geohydroinformatik B-9
Aminzadeh, Milad
Geohydroinformatik B-9
Mirfasihi, Sorosh
Or, Dani
Patzke, Justus
Wasserbau B-10
Fröhle, Peter
Wasserbau B-10
Keshmiri, Amir
Shokri, Nima
Geohydroinformatik B-9
TORE-DOI
10.15480/882.18703
TORE-URI
https://hdl.handle.net/11420/65136
Journal
Water resources research
Volume
62
Issue
9
Article Number
e2026WR043631
Citation
Water Resources Research 62 (9): e2026WR043631 (2026)
Publisher DOI
10.1029/2026WR043631
Scopus ID
2-s2.0-105050668860
Publisher
Wiley
Peer Reviewed
true
In contrast to the wealth of information on evaporation dynamics from placid water surfaces such as lakes and reservoirs, estimating water evaporation from turbulent surfaces of streams remains a challenge. Evidence suggests considerable differences in evaporation rates from flowing water bodies relative to placid surfaces. Here, we experimentally investigate how flow characteristics (velocity and turbulence) and boundary conditions (wind and radiation) regulate evaporation from flowing water surfaces by using a controlled laboratory flume to isolate key hydrodynamic–atmospheric interactions relevant to streams and rivers. We used a closed flume (7.6 m length, 0.31 m width, and 0.5 m depth) imposing different boundary conditions over the test section of 1.5 m in length while other parts of the flume were covered to prevent evaporative losses. Our results demonstrate that the effect of turbulence on evaporation depends on the temperature profile of the water body and redistribution of radiative heat with turbulent mixing highlighting that evaporation emerges from a nonlinear coupling between hydrodynamic mixing and energy availability. Under solar radiation, increased water flow and turbulence can reduce evaporation by suppressing the formation of a warm surface layer and redistributing absorbed heat in depth of the water column. Without shortwave radiation flux, however, enhanced surface velocity and turbulent mixing may cause significant enhancement in evaporation rates up to 2–5 times that of placid water surfaces. Numerical simulations indicate that enhanced surface turbulence and wave activity increase interfacial roughness and shear, regulating the vapor boundary layer and producing spatially heterogeneous and intermittent vapor fluxes. The study offers novel insights into evaporation from wavy and turbulent flowing water surfaces for a better understanding of evaporation from riverine networks across flow regimes and climatic conditions.
Subjects
evaporation dynamics
flowing water surfaces
laboratory flume
numerical simulation
rivers and streams
turbulence
DDC Class
551: Geology, Hydrology Meteorology
Funding(s)
United Nations University Hub on Engineering to Face Climate Change at Hamburg University of Technology
Lizenz
https://creativecommons.org/licenses/by/4.0/
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