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contributor authorWeil, Jeffrey C.
date accessioned2017-06-09T16:18:23Z
date available2017-06-09T16:18:23Z
date copyright2008/09/01
date issued2008
identifier issn1558-8424
identifier otherams-65412.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206635
description abstractA slightly simplified form of Thomson?s Lagrangian stochastic model (LSM) is presented for dispersion applications in three-dimensional (3D) flow fields. It is found that the Lagrangian velocity of a particle in 3D inhomogeneous Gaussian turbulence can be decomposed into the local Eulerian mean velocity UEi at the particle position and a velocity perturbation u?i. The Eulerian mean wind can be predicted by 3D wind field models, whereas the u?i is obtained from Thomson?s model and depends on the turbulence field. The UEi, u?i decomposition was used earlier in a two-dimensional particle model for a canopy (by Flesch and Wilson) and in models with 3D mean winds but with u?i based on LSM forms differing from that of Thomson. This note shows that the UEi, u?i decomposition is consistent with Thomson?s LSM for general 3D flow fields and is a simpler solution that should lead to improved computational efficiency for dispersion applications.
publisherAmerican Meteorological Society
titleLinking a Lagrangian Particle Dispersion Model with Three-Dimensional Eulerian Wind Field Models
typeJournal Paper
journal volume47
journal issue9
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/2007JAMC1764.1
journal fristpage2463
journal lastpage2467
treeJournal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 009
contenttypeFulltext


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