Journal of the Meteorological Society of Japan. Ser. II
Online ISSN : 2186-9057
Print ISSN : 0026-1165
ISSN-L : 0026-1165
Evaporation by Natural Convection
G. YamamotoA. Miura
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1949 Volume 27 Issue 11 Pages 342-345

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Abstract
From the analogy between heat transfer and evaporation, the rate of evaporation from a finite pan by natural convection was obtained as follows:
where E is the rate of evaporation in g•cm-2•see-1, C0, C are vapour concentrations at the surface of water and in the air respectively, _??_θ0, θ0, θ being temperatures at the surface of water and in the air respectively, d is diffusivity, _??_; kinematic viscosity, β; expansion coefficient of air, g; acceleration of gravity and x is the radius of the pan in cm.
Experiments were carried out by using a pan of radius 1.83cm. The range of _??_=θ0 observed was from 0.1° to 50°C, in which θ was about 20°C. The experimental result was expressed by while the theoretical formula for the pan at θ=20°C is
Both results agree fairly well, but the experimental result gives about 21% smaller rate of evaporation than the theoretical formula.
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