Computation of Ground Surface Conduction Heat Flux by Fourier Analysis of Surface Temperature

dc.contributor.author	Cautenet, Guy
dc.contributor.author	Legrand, Michel
dc.contributor.author	Coulibaly, Yaya
dc.contributor.author	Boutin, Christian
dc.date.accessioned	2017-06-09T14:01:00Z
dc.date.available	2017-06-09T14:01:00Z
dc.date.copyright	1986/03/01
dc.date.issued	1986
dc.identifier.issn	0733-3021
dc.identifier.other	ams-10963.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4146138
dc.description.abstract	A method for computing the ground surface heat flux density is tested at two places in West Africa during the rainy season and during the dry season. This method is based upon the Fourier analysis of the experimental ground surface temperature. The only required parameter is the soil thermal inertia. The results of these calculations agree with the measurements. This method avoids the use of empirical formulas relating the ground heat flux density to other terms of the surface energy budget. It is shown that these relations are not universal.
dc.publisher	American Meteorological Society
dc.title	Computation of Ground Surface Conduction Heat Flux by Fourier Analysis of Surface Temperature
dc.type	Journal Paper
dc.journal.volume	25
dc.journal.issue	3
dc.journal.title	Journal of Climate and Applied Meteorology
dc.identifier.doi	10.1175/1520-0450(1986)025<0277:COGSCH>2.0.CO;2
dc.journal.fristpage	277
dc.journal.lastpage	283
dc.tree	Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 003
dc.contenttype	Fulltext