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contributor authorBusinger, J. A.
contributor authorMiyake, M.
contributor authorDyer, A. J.
contributor authorBradley, E. F.
date accessioned2017-06-09T16:53:02Z
date available2017-06-09T16:53:02Z
date copyright1967/12/01
date issued1967
identifier issn0021-8952
identifier otherams-7592.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218311
description abstractThe results of a heat flux comparison experiment carried out at Hay, New South Wales, Australia, during May 1966 using a sonic anemometer thermometer (SAT), Fluxatron and Evapotron are reported. The instruments agree with each other to within a factor of 2 for individual runs. The large fluctuations from run to run of the individual estimates are mainly caused by the fact that the Eulerian point average does not provide an adequate statistical sample of the heat flux. This point is illustrated by the non-stationary behavior of the instantaneous product of vertical wind and temperature. As auxiliary results, values of σw/u* and σT/T* have been obtained which are somewhat higher than, but in general agreement with, observations reported by Mordukhovich and Zwang.
publisherAmerican Meteorological Society
titleOn the Direct Determination of the Turbulent Heat Flux Near the Ground
typeJournal Paper
journal volume6
journal issue6
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1967)006<1025:OTDDOT>2.0.CO;2
journal fristpage1025
journal lastpage1032
treeJournal of Applied Meteorology:;1967:;volume( 006 ):;issue: 006
contenttypeFulltext


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