Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the Ground

A simple Lagrangian stochastic (LS) dispersion model was used to investigate atmospheric dispersion in the lower atmospheric boundary layer, for near-surface sources. The sensitivity of ground-level concentration to numerical errors was revealed. Numerical treatments of inhomogeneous atmospheric tur...

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Main Author: Qing Huo Xuhui Cai
Format: Article
Language:English
Published: Chinese Geoscience Union 2014-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v251p077.pdf
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spelling doaj-66c9720a56f143ae8e76238f2d5067d32020-11-24T22:14:43ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802014-01-0125107710.3319/TAO.2013.09.23.01(A)1200Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the GroundQing Huo Xuhui CaiA simple Lagrangian stochastic (LS) dispersion model was used to investigate atmospheric dispersion in the lower atmospheric boundary layer, for near-surface sources. The sensitivity of ground-level concentration to numerical errors was revealed. Numerical treatments of inhomogeneous atmospheric turbulence and surface reflection in Lagrangian trajectory calculations may cause non-negligible overestimates of ground-level concentration for elevated sources, although these errors become trivial for surface sources and for concentrations above the ground-level. Using a numerical error-correction scheme, the LS model was evaluated against an analytical model. Close agreement was found between the two models in predicting ground-level concentrations for dispersions in the surface layer. LS simulations for an elevated source were also conducted. A scaling scheme was proposed to normalize the dispersion results, by including the source height as a scaling length. The relationships between the normalized surface concentration and downwind distance were distinguished by atmospheric stabilities. In the near-field, the distance of peak ground-level concentration was 0.5, 1.0, and 2.0 times zs U/u*, where zs is the source height, U is the mean wind speed at height 10 m, and u* is the friction velocity, for unstable, neutral and stable atmospheric stability conditions, respectively. In the far-field, the concentration approached approximately the ¡§-3/2¡¨, ¡§-1¡¨ and ¡§-2/3¡¨ law for unstable, neutral and stable atmospheres respectively. http://tao.cgu.org.tw/images/attachments/v251p077.pdf DispersionElevated sourceGround-level concentrationLagrangian stochastic model
collection DOAJ
language English
format Article
sources DOAJ
author Qing Huo Xuhui Cai
spellingShingle Qing Huo Xuhui Cai
Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the Ground
Terrestrial, Atmospheric and Oceanic Sciences
Dispersion
Elevated source
Ground-level concentration
Lagrangian stochastic model
author_facet Qing Huo Xuhui Cai
author_sort Qing Huo Xuhui Cai
title Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the Ground
title_short Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the Ground
title_full Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the Ground
title_fullStr Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the Ground
title_full_unstemmed Lagrangian Stochastic Simulation of Atmospheric Dispersion from Sources near the Ground
title_sort lagrangian stochastic simulation of atmospheric dispersion from sources near the ground
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2014-01-01
description A simple Lagrangian stochastic (LS) dispersion model was used to investigate atmospheric dispersion in the lower atmospheric boundary layer, for near-surface sources. The sensitivity of ground-level concentration to numerical errors was revealed. Numerical treatments of inhomogeneous atmospheric turbulence and surface reflection in Lagrangian trajectory calculations may cause non-negligible overestimates of ground-level concentration for elevated sources, although these errors become trivial for surface sources and for concentrations above the ground-level. Using a numerical error-correction scheme, the LS model was evaluated against an analytical model. Close agreement was found between the two models in predicting ground-level concentrations for dispersions in the surface layer. LS simulations for an elevated source were also conducted. A scaling scheme was proposed to normalize the dispersion results, by including the source height as a scaling length. The relationships between the normalized surface concentration and downwind distance were distinguished by atmospheric stabilities. In the near-field, the distance of peak ground-level concentration was 0.5, 1.0, and 2.0 times zs U/u*, where zs is the source height, U is the mean wind speed at height 10 m, and u* is the friction velocity, for unstable, neutral and stable atmospheric stability conditions, respectively. In the far-field, the concentration approached approximately the ¡§-3/2¡¨, ¡§-1¡¨ and ¡§-2/3¡¨ law for unstable, neutral and stable atmospheres respectively.
topic Dispersion
Elevated source
Ground-level concentration
Lagrangian stochastic model
url http://tao.cgu.org.tw/images/attachments/v251p077.pdf
work_keys_str_mv AT qinghuoxuhuicai lagrangianstochasticsimulationofatmosphericdispersionfromsourcesneartheground
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