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Dependence of Convective Heat Flux Calculations on Roughness Lengths

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dc.contributor.author Schieldge, John P. en_US
dc.date.accessioned 2004-10-04T21:26:29Z
dc.date.available 2004-10-04T21:26:29Z
dc.date.issued 1995-11 en_US
dc.identifier.citation Boundary-Layer Meteorology en_US
dc.identifier.clearanceno 95-1560 en_US
dc.identifier.uri http://hdl.handle.net/2014/32219
dc.description.abstract The zero plane displacement height (d) and aerodynamic roughness length (z0) can be determined separately for momentum, heat, and humidity by using a procedure based on the Levenberg-Marquardt method for solving non-linear equations. This procedure is used to analyze profile data previously collected by Lo (1977) in a forested area in Canada and by Morgan et al (1971) on a field at the University of California at Davis (UCD) in the United States. The UCD data base is used to show the effects of allowing for different roughness lengths (zom,z0h,z0q) in calculating sensible and latent heat flux densities from bulk transfer coefficients. en_US
dc.format.extent 502108 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other Convective Heat en_US
dc.title Dependence of Convective Heat Flux Calculations on Roughness Lengths en_US


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