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A generalized combination equation derived from a multi-layer micrometeorological model

✍ Scribed by Jean-Paul Lhomme


Book ID
104629341
Publisher
Springer
Year
1988
Tongue
English
Weight
684 KB
Volume
45
Category
Article
ISSN
0006-8314

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✦ Synopsis


The discrete multi-layer model originally devised by is used as a theoretical basis to describe the vegetation-atmosphere interaction. Mathematical development of the basic equations yields Ohm's law-type formulae for sensible and latent heat fluxes from which it is possible to derive a combination equation very close in form to Penman-Monteith's equation. A bulk aerodynamic resistance and a bulk stomata1 resistance can be defined and expressed in terms of the elementary resistances of the multi-layer model. This new combination equation offers an alternative to the attempts undertaken by Shuttleworth (1976) to unify multi-layer and single-layer approaches.


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## Abstract A mathematical model was developed for three‐dimensional (3‐D) simulation of free surface flows. In this model, the flow depth is divided into a number of layers and shallow water equations are integrated in each layer to derive the hydrodynamic equations. To give a general form to this