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contributor authorYamada, Tetsuji
contributor authorMellor, George
date accessioned2017-06-09T14:18:35Z
date available2017-06-09T14:18:35Z
date copyright1975/12/01
date issued1975
identifier issn0022-4928
identifier otherams-16960.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152801
description abstractPreviously, the authors have studied a hierarchy of turbulent boundary layer models, all based on the same closure assumptions for the triple turbulence moments. The models differ in complexity by virtue of a systematic process of neglecting certain of the tendency and diffusion terms in the dynamic equations for the turbulent moments. Based on this work a Level 3 model was selected as one which apparently sacrificed little predictive accuracy, but which afforded considerable numerical simplification relative to the more complex Level 4 model. An earlier paper had demonstrated that the model produced similarity solutions in near agreement with surface, constant flux data. In this paper, simulators from the Level 3 model are compared with two days of Wangara atmospheric boundary layer data (Clarke et al., 1971). In this comparison, there is an easily identified error introduced by our inability to include advection of momentum in the calculation since these terms were not measured. Otherwise, the calculated results and the observational data appear to he in close agreement.
publisherAmerican Meteorological Society
titleA Simulation of the Wangara Atmospheric Boundary Layer Data
typeJournal Paper
journal volume32
journal issue12
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1975)032<2309:ASOTWA>2.0.CO;2
journal fristpage2309
journal lastpage2329
treeJournal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 012
contenttypeFulltext


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