Titlebook: Stochastic Lagrangian Models of Turbulent Diffusion; Howard C. Rodean Book 1996 American Meteorological Society 1996 Convective boundary l

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書(shū)目名稱(chēng)Stochastic Lagrangian Models of Turbulent Diffusion影響因子(影響力)

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書(shū)目名稱(chēng)Stochastic Lagrangian Models of Turbulent Diffusion被引頻次

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書(shū)目名稱(chēng)Stochastic Lagrangian Models of Turbulent Diffusion讀者反饋

書(shū)目名稱(chēng)Stochastic Lagrangian Models of Turbulent Diffusion讀者反饋學(xué)科排名

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Criteria for Stochastic Models of Turbulent Diffusion,e diffusion equation and Thomson’s (1987) well-mixed criterion. It is appropriate at this point to review the several criteria that have been proposed. These were the subject of Thomson’s classic paper in which he considered the following five:.Thomson showed in section 3 of his paper that a general

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Application to the Convective Boundary Layer,roximation. A major exception is the convective boundary layer (CBL) because the persistent updrafts and downdrafts dominate the vertical flow. The resultant trajectory of a passive tracer cannot, therefore, be regarded as a superposition of independent increments as in Eqs. (9.8c) and (9.10b), for

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Parameterization of Turbulence Statistics for Model Inputs,isplacement model (RDM)1 are 1) the variance of the turbulent velocity fluctuations (e.g., σ.) and 2) either the local decorrelation timescale . or the rate of dissipation of the turbulence kinetic energy .. The inputs σ. and . or . are sufficient for diffusion in one dimension, the vertical. In mor

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