Evaluation of a new convective cloud field model: precipitation over the maritime continent

A convective cloud field model (CCFM) is substituted for a standard mass flux parameterisation of convective clouds in a limited area atmospheric model (REMO) and is tested for a whole annual cycle (July 1997 to June 1998) over the West Pacific Maritime Continent. REMO with CCFM is run in 0.5-degree...

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Main Authors: H.-F. Graf, J. Yang
Format: Article
Language:English
Published: Copernicus Publications 2007-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/7/409/2007/acp-7-409-2007.pdf
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spelling doaj-c743612cc6c447a79e7e2c54a33318632020-11-25T01:08:50ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242007-01-0172409421Evaluation of a new convective cloud field model: precipitation over the maritime continentH.-F. GrafJ. YangA convective cloud field model (CCFM) is substituted for a standard mass flux parameterisation of convective clouds in a limited area atmospheric model (REMO) and is tested for a whole annual cycle (July 1997 to June 1998) over the West Pacific Maritime Continent. REMO with CCFM is run in 0.5-degree resolution and the model at the lateral boundaries is forced 6-hourly by ECMWF reanalysis data. Simulated precipitation from runs with the standard convection parameterisation and with CCFM is compared against two sets of observations. The use of CCFM clearly improves the simulated precipitation patterns and total rainfall over the whole model domain. The distribution between large-scale and convective precipitation becomes more realistic. CCFM shows to be a useful concept to describe convective cloud spectra in atmospheric models, although there are still similar problems with occasionally extreme precipitation as in the original set-up of REMO.http://www.atmos-chem-phys.net/7/409/2007/acp-7-409-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H.-F. Graf
J. Yang
spellingShingle H.-F. Graf
J. Yang
Evaluation of a new convective cloud field model: precipitation over the maritime continent
Atmospheric Chemistry and Physics
author_facet H.-F. Graf
J. Yang
author_sort H.-F. Graf
title Evaluation of a new convective cloud field model: precipitation over the maritime continent
title_short Evaluation of a new convective cloud field model: precipitation over the maritime continent
title_full Evaluation of a new convective cloud field model: precipitation over the maritime continent
title_fullStr Evaluation of a new convective cloud field model: precipitation over the maritime continent
title_full_unstemmed Evaluation of a new convective cloud field model: precipitation over the maritime continent
title_sort evaluation of a new convective cloud field model: precipitation over the maritime continent
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2007-01-01
description A convective cloud field model (CCFM) is substituted for a standard mass flux parameterisation of convective clouds in a limited area atmospheric model (REMO) and is tested for a whole annual cycle (July 1997 to June 1998) over the West Pacific Maritime Continent. REMO with CCFM is run in 0.5-degree resolution and the model at the lateral boundaries is forced 6-hourly by ECMWF reanalysis data. Simulated precipitation from runs with the standard convection parameterisation and with CCFM is compared against two sets of observations. The use of CCFM clearly improves the simulated precipitation patterns and total rainfall over the whole model domain. The distribution between large-scale and convective precipitation becomes more realistic. CCFM shows to be a useful concept to describe convective cloud spectra in atmospheric models, although there are still similar problems with occasionally extreme precipitation as in the original set-up of REMO.
url http://www.atmos-chem-phys.net/7/409/2007/acp-7-409-2007.pdf
work_keys_str_mv AT hfgraf evaluationofanewconvectivecloudfieldmodelprecipitationoverthemaritimecontinent
AT jyang evaluationofanewconvectivecloudfieldmodelprecipitationoverthemaritimecontinent
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