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contributor authorHelmis, C. G.
contributor authorAsimakopoulos, D. N.
contributor authorLalas, D. P.
contributor authorMoulsley, T. J.
date accessioned2017-06-09T13:59:45Z
date available2017-06-09T13:59:45Z
date copyright1983/09/01
date issued1983
identifier issn0733-3021
identifier otherams-10580.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145713
description abstractExperimental results of simultaneous measurements of temperature differences in the streamwise, lateral and vertical directions during convective, new-neutral and stable conditions in the atmospheric boundary layer of an urban site are presented and discussed. The lateral and vertical temperature difference variances are found to be almost equal regardless of the conditions but only agree with the streamwise difference variance in convective or rear-neutral conditions. This points out the need for further investigation of the effects of stratification on the scalar fields. When local isotropy is satisfied, the difference spectra are shown to follow the theoretical behavior derived by Van Atta (1977).for temperature gradients in the inertial subrange.
publisherAmerican Meteorological Society
titleOn the Local Isotropy of the Temperature Field in an Urban Area
typeJournal Paper
journal volume22
journal issue9
journal titleJournal of Climate and Applied Meteorology
identifier doi10.1175/1520-0450(1983)022<1594:OTLIOT>2.0.CO;2
journal fristpage1594
journal lastpage1601
treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 009
contenttypeFulltext


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