Evaporation rates across a convective air boundary layer are dominated by diffusion

Key Points The contributions of diffusion and advection to evaporative flux are quantified Diffusion dominates evaporation flux from partially wet surfaces Surface water content‐dependent evaporative resistance expression is developed The relative contributions of advection and diffusion to isotherm...

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Veröffentlicht in:	Water resources research 2013-03, Vol.49 (3), p.1602-1610
Hauptverfasser:	Haghighi, E., Shahraeeni, E., Lehmann, P., Or, D.
Format:	Artikel
Sprache:	eng
Schlagworte:	Advection Boundary conditions Boundary layer Boundary layers Diffusion Drying Evaporation Evaporation rate evaporative resistance Mass transfer Meteorology Pores porous media Soil types Surface water Water content
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