Application of a simple finite difference model for estimating evaporation from open water

In estimating the evaporation from open water, the challenge is to accurately quantify the change in heat stored in the water body. A simple finite difference model is described and a comparison made between measured values of water temperature and evaporation, from a reservoir in southeast England,...

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Bibliographic Details
Published inJournal of hydrology (Amsterdam) Vol. 255; no. 1; pp. 253 - 259
Main Authors Finch, J.W, Gash, J.H.C
Format Journal Article
LanguageEnglish
Published Amsterdam Elsevier B.V 02.01.2002
Elsevier Science
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Summary:In estimating the evaporation from open water, the challenge is to accurately quantify the change in heat stored in the water body. A simple finite difference model is described and a comparison made between measured values of water temperature and evaporation, from a reservoir in southeast England, and the values predicted by an equilibrium temperature model. The values predicted by the new model are in excellent agreement with the measurements and are closer to the measured values than those predicted by the equilibrium temperature model. The difference in performance is attributed to improved methods used for calculating the net radiation and the wind function. The simpler formulation of the finite difference model is considered to offset the disadvantage of the greater number of calculations required.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0022-1694
1879-2707
DOI:10.1016/S0022-1694(01)00511-X