Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling

Numerical diffusion induced by advection has a large influence on concentration of substances in atmospheric composition models. At coarse resolution numerical effects dominate, whereas at increasing model resolution a description of physical diffusion is needed. A method to investigate the effects...

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Main Authors: M. D'Isidoro, A. Maurizi, F. Tampieri
Format: Article
Language:English
Published: Copernicus Publications 2010-03-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/10/2737/2010/acp-10-2737-2010.pdf
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spelling doaj-217e0ab27c174aa4aa28b776be5256f32020-11-24T23:37:28ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242010-03-0110627372743Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modellingM. D'IsidoroA. MauriziF. TampieriNumerical diffusion induced by advection has a large influence on concentration of substances in atmospheric composition models. At coarse resolution numerical effects dominate, whereas at increasing model resolution a description of physical diffusion is needed. A method to investigate the effects of changing resolution and Courant number is defined here and is applied to the WAF advection scheme (used in BOLCHEM), evidencing a sub-diffusive process. The spread rate from an instantaneous source caused by numerical diffusion is compared to that produced by the physical diffusion necessary to simulate unresolved turbulent motions. The time at which the physical diffusion process overpowers the numerical spread is estimated, and it is shown to reduce as the resolution increases, and to increase with wind velocity. http://www.atmos-chem-phys.net/10/2737/2010/acp-10-2737-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. D'Isidoro
A. Maurizi
F. Tampieri
spellingShingle M. D'Isidoro
A. Maurizi
F. Tampieri
Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling
Atmospheric Chemistry and Physics
author_facet M. D'Isidoro
A. Maurizi
F. Tampieri
author_sort M. D'Isidoro
title Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling
title_short Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling
title_full Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling
title_fullStr Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling
title_full_unstemmed Effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling
title_sort effects of resolution on the relative importance of numerical and physical horizontal diffusion in atmospheric composition modelling
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2010-03-01
description Numerical diffusion induced by advection has a large influence on concentration of substances in atmospheric composition models. At coarse resolution numerical effects dominate, whereas at increasing model resolution a description of physical diffusion is needed. A method to investigate the effects of changing resolution and Courant number is defined here and is applied to the WAF advection scheme (used in BOLCHEM), evidencing a sub-diffusive process. The spread rate from an instantaneous source caused by numerical diffusion is compared to that produced by the physical diffusion necessary to simulate unresolved turbulent motions. The time at which the physical diffusion process overpowers the numerical spread is estimated, and it is shown to reduce as the resolution increases, and to increase with wind velocity.
url http://www.atmos-chem-phys.net/10/2737/2010/acp-10-2737-2010.pdf
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