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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Chinese Geoscience Union
2014-01-01
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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
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work_keys_str_mv |
AT qinghuoxuhuicai lagrangianstochasticsimulationofatmosphericdispersionfromsourcesneartheground |
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1725797400469045248 |