Statistical representation of mountain shading

Shadows cast by the mountains themselves have a strong influence on the surface energy balance of mountainous regions. If the influence of shadows is to be included on sub-grid scales in a surface energy balance model, a statistical representation has to be used. Slope components calculated from d...

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Main Author: R. Essery
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/8/1047/2004/hess-8-1047-2004.pdf
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author R. Essery
R. Essery
author_facet R. Essery
R. Essery
author_sort R. Essery
collection DOAJ
description Shadows cast by the mountains themselves have a strong influence on the surface energy balance of mountainous regions. If the influence of shadows is to be included on sub-grid scales in a surface energy balance model, a statistical representation has to be used. Slope components calculated from digital elevation models of areas in North Wales and the French Alps are found to have double-exponential distributions. From this result, expressions are developed for the fractions of the areas that will be either self-shaded or shaded by remote topography as functions of solar elevation and time of day. These expressions are in good agreement with results from a terrain shading model. </p> <p style='line-height: 20px;'><b>Keywords: </b>solar radiation, topography, surface energy balance, statistical parameterisation
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spelling doaj.art-8b7a6ced75734a6bbd1385fab5e4cd7e2022-12-21T23:21:48ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382004-01-018610471052Statistical representation of mountain shadingR. EsseryR. EsseryShadows cast by the mountains themselves have a strong influence on the surface energy balance of mountainous regions. If the influence of shadows is to be included on sub-grid scales in a surface energy balance model, a statistical representation has to be used. Slope components calculated from digital elevation models of areas in North Wales and the French Alps are found to have double-exponential distributions. From this result, expressions are developed for the fractions of the areas that will be either self-shaded or shaded by remote topography as functions of solar elevation and time of day. These expressions are in good agreement with results from a terrain shading model. </p> <p style='line-height: 20px;'><b>Keywords: </b>solar radiation, topography, surface energy balance, statistical parameterisationhttp://www.hydrol-earth-syst-sci.net/8/1047/2004/hess-8-1047-2004.pdf
spellingShingle R. Essery
R. Essery
Statistical representation of mountain shading
Hydrology and Earth System Sciences
title Statistical representation of mountain shading
title_full Statistical representation of mountain shading
title_fullStr Statistical representation of mountain shading
title_full_unstemmed Statistical representation of mountain shading
title_short Statistical representation of mountain shading
title_sort statistical representation of mountain shading
url http://www.hydrol-earth-syst-sci.net/8/1047/2004/hess-8-1047-2004.pdf
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