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dc.contributor.authorWeill, A.
dc.contributor.authorKlapisz, C.
dc.contributor.authorStrauss, B.
dc.contributor.authorBaudin, F.
dc.contributor.authorJaupart, C.
dc.contributor.authorVan Grunderbeeck, P.
dc.contributor.authorGoutorbe, J. P.
dc.date.accessioned2017-06-09T17:40:22Z
dc.date.available2017-06-09T17:40:22Z
dc.date.copyright1980/02/01
dc.date.issued1979
dc.identifier.issn0021-8952
dc.identifier.otherams-9857.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233391
dc.description.abstractThe vertical velocity variance during convective activity was measured with an acoustic Doppler sounder. Here we show that this technique provides measurement of the heat flux profile in the well-mixed surface layer and gives a reference height h? related to the inversion height ZI during the mornings. The paper also shows that the structure function of temperature fluctuations CT2 can be obtained by these measurements using the Kaimal et al. (1976) formula.
dc.publisherAmerican Meteorological Society
dc.titleMeasuring Heat Flux and Structure Functions of Temperature Fluctuations with an Acoustic Doppler Sodar
dc.typeJournal Paper
dc.journal.volume19
dc.journal.issue2
dc.journal.titleJournal of Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1980)019<0199:MHFASF>2.0.CO;2
dc.journal.fristpage199
dc.journal.lastpage205
dc.treeJournal of Applied Meteorology:;1979:;volume( 019 ):;issue: 002
dc.contenttypeFulltext


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