Lagrangian Dispersion Model for Nonneutrally Buoyant PlumesSource: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 003::page 427Author:Yamada, Tetsuji
DOI: 10.1175/1520-0450(2000)039<0427:LDMFNB>2.0.CO;2Publisher: American Meteorological Society
Abstract: A capability to address positive and negative buoyancy was added to the Higher-Order Turbulence Model for Atmospheric Circulation?Random Puff Transport and Diffusion (HOTMAC?RAPTAD) modeling system. The modeling system was applied to simulate dense gas plumes, and the modeled concentrations were compared with observations reported in the Modelers? Data Archives (MDA). Sampling sites reported in MDA were located mostly 50?800 m from the source over flat terrain. To detect a peak concentration, RAPTAD sampling sites were placed on the arcs whose radii correspond to the sampling distance reported in MDA. Concentration averaging time for a peak concentration was varied from 1 to 600 s. RAPTAD simulation time varied from 4 to 30 min. The overall performance of the current model in terms of geometric mean biases, geometric variances, and residual plots was found to be at least as good as those of the better models examined previously with the same dataset.
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| contributor author | Yamada, Tetsuji | |
| date accessioned | 2017-06-09T14:07:21Z | |
| date available | 2017-06-09T14:07:21Z | |
| date copyright | 2000/03/01 | |
| date issued | 2000 | |
| identifier issn | 0894-8763 | |
| identifier other | ams-12827.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4148209 | |
| description abstract | A capability to address positive and negative buoyancy was added to the Higher-Order Turbulence Model for Atmospheric Circulation?Random Puff Transport and Diffusion (HOTMAC?RAPTAD) modeling system. The modeling system was applied to simulate dense gas plumes, and the modeled concentrations were compared with observations reported in the Modelers? Data Archives (MDA). Sampling sites reported in MDA were located mostly 50?800 m from the source over flat terrain. To detect a peak concentration, RAPTAD sampling sites were placed on the arcs whose radii correspond to the sampling distance reported in MDA. Concentration averaging time for a peak concentration was varied from 1 to 600 s. RAPTAD simulation time varied from 4 to 30 min. The overall performance of the current model in terms of geometric mean biases, geometric variances, and residual plots was found to be at least as good as those of the better models examined previously with the same dataset. | |
| publisher | American Meteorological Society | |
| title | Lagrangian Dispersion Model for Nonneutrally Buoyant Plumes | |
| type | Journal Paper | |
| journal volume | 39 | |
| journal issue | 3 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(2000)039<0427:LDMFNB>2.0.CO;2 | |
| journal fristpage | 427 | |
| journal lastpage | 436 | |
| tree | Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 003 | |
| contenttype | Fulltext |