Modelling atmospheric dry deposition in urban areas using an urban canopy approach

Atmospheric dry deposition is typically modelled using an average roughness length, which depends on land use. This classical roughness-length approach cannot account for the spatial variability of dry deposition in complex settings such as urban areas. Urban canopy models have been developed...

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Main Authors: N. Cherin, Y. Roustan, L. Musson-Genon, C. Seigneur
Format: Article
Language:English
Published: Copernicus Publications 2015-03-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/8/893/2015/gmd-8-893-2015.pdf
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spelling doaj-59072837370f483aa41d9dd2ab5b0d3b2020-11-24T22:55:58ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032015-03-018389391010.5194/gmd-8-893-2015Modelling atmospheric dry deposition in urban areas using an urban canopy approachN. Cherin0Y. Roustan1L. Musson-Genon2C. Seigneur3CEREA, Joint Laboratory École des Ponts ParisTech and EDF R&D, Université Paris-Est, 77455 Marne-la-Vallée, FranceCEREA, Joint Laboratory École des Ponts ParisTech and EDF R&D, Université Paris-Est, 77455 Marne-la-Vallée, FranceCEREA, Joint Laboratory École des Ponts ParisTech and EDF R&D, Université Paris-Est, 77455 Marne-la-Vallée, FranceCEREA, Joint Laboratory École des Ponts ParisTech and EDF R&D, Université Paris-Est, 77455 Marne-la-Vallée, FranceAtmospheric dry deposition is typically modelled using an average roughness length, which depends on land use. This classical roughness-length approach cannot account for the spatial variability of dry deposition in complex settings such as urban areas. Urban canopy models have been developed to parametrise momentum and heat transfer. We extend this approach here to mass transfer, and a new dry deposition model based on the urban canyon concept is presented. It uses a local mixing-length parametrisation of turbulence within the canopy, and a description of the urban canopy via key parameters to provide spatially distributed dry deposition fluxes. Three different flow regimes are distinguished in the urban canyon depending on the height-to-width ratio of built areas: isolated roughness flow, wake interference flow and skimming flow. Differences between the classical roughness-length model and the model developed here are investigated. Sensitivity to key parameters are discussed. This approach provides spatially distributed dry deposition fluxes that depend on surfaces (streets, walls, roofs) and flow regimes (recirculation and ventilation) within the urban area.http://www.geosci-model-dev.net/8/893/2015/gmd-8-893-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. Cherin
Y. Roustan
L. Musson-Genon
C. Seigneur
spellingShingle N. Cherin
Y. Roustan
L. Musson-Genon
C. Seigneur
Modelling atmospheric dry deposition in urban areas using an urban canopy approach
Geoscientific Model Development
author_facet N. Cherin
Y. Roustan
L. Musson-Genon
C. Seigneur
author_sort N. Cherin
title Modelling atmospheric dry deposition in urban areas using an urban canopy approach
title_short Modelling atmospheric dry deposition in urban areas using an urban canopy approach
title_full Modelling atmospheric dry deposition in urban areas using an urban canopy approach
title_fullStr Modelling atmospheric dry deposition in urban areas using an urban canopy approach
title_full_unstemmed Modelling atmospheric dry deposition in urban areas using an urban canopy approach
title_sort modelling atmospheric dry deposition in urban areas using an urban canopy approach
publisher Copernicus Publications
series Geoscientific Model Development
issn 1991-959X
1991-9603
publishDate 2015-03-01
description Atmospheric dry deposition is typically modelled using an average roughness length, which depends on land use. This classical roughness-length approach cannot account for the spatial variability of dry deposition in complex settings such as urban areas. Urban canopy models have been developed to parametrise momentum and heat transfer. We extend this approach here to mass transfer, and a new dry deposition model based on the urban canyon concept is presented. It uses a local mixing-length parametrisation of turbulence within the canopy, and a description of the urban canopy via key parameters to provide spatially distributed dry deposition fluxes. Three different flow regimes are distinguished in the urban canyon depending on the height-to-width ratio of built areas: isolated roughness flow, wake interference flow and skimming flow. Differences between the classical roughness-length model and the model developed here are investigated. Sensitivity to key parameters are discussed. This approach provides spatially distributed dry deposition fluxes that depend on surfaces (streets, walls, roofs) and flow regimes (recirculation and ventilation) within the urban area.
url http://www.geosci-model-dev.net/8/893/2015/gmd-8-893-2015.pdf
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