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dc.contributor.authorSun, Wen-Yih
dc.contributor.authorChang, Chiao-Zen
dc.date.accessioned2017-06-09T14:01:24Z
dc.date.available2017-06-09T14:01:24Z
dc.date.copyright1986/10/01
dc.date.issued1986
dc.identifier.issn0733-3021
dc.identifier.otherams-11065.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146252
dc.description.abstractA simple turbulence model is used to study the moist convective boundary layer, in which a prognostic equation is applied to calculate the turbulent kinetic energy E. An observational length scale of the vertical velocity component, l, is used in the mixed layer, while a length scale associated with gravity waves is applied in the stable layer. The eddy coefficient is proportional to El. This model simulates well the temperature, mixing ratio and mean wind observed in the Wangara experiments. The turbulent kinetic energy and eddy fluxes generated are also in good agreement with those observed, as well as with those obtained from other more complicated models. Furthermore, the parameterization and results generated are used in a pollution model, which will be presented in Part II of this study.
dc.publisherAmerican Meteorological Society
dc.titleDiffusion Model for a Convective Layer. Part I: Numerical Simulation of Convective Boundary Layer
dc.typeJournal Paper
dc.journal.volume25
dc.journal.issue10
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1986)025<1445:DMFACL>2.0.CO;2
dc.journal.fristpage1445
dc.journal.lastpage1453
dc.treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 010
dc.contenttypeFulltext


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