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dc.contributor.authorGerard, L.
dc.coverage.temporal21st century
dc.date2007
dc.date.accessioned2016-03-07T16:16:56Z
dc.date.accessioned2021-12-09T09:53:42Z
dc.date.available2016-03-07T16:16:56Z
dc.date.available2021-12-09T09:53:42Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/8723
dc.descriptionThe integration into a coherent package of the main ”moist” parametrizations – deep convection, resolved condensation, microphysics – of a limited area model is presented. The development of the package is aimed at solving efficiently the problem of combining ’resolved’ and ’subgrid’ condensation at all resolutions, in particular the range between 10 km and 2 km where deep convection is partly resolved, partly subgrid. The different schemes of the package are called in cascade, with intermediate updating of internal variables, so that for instance the initial profiles passed to the deep-convection scheme are already balanced with respect to resolved condensation effects. Further on, the clean separation of the contributions to the closure of the updraught and downdraught from the initial vertical profile from which they evolve prevents double counting. The convective parametrization works with a prognostic mass-flux scheme, and acts on the resolved variables through condensation and convective transport. It detrains condensates that are added to the prognostic resolved condensates. A sensitivity study in a single-column model, and further validation in three-dimensional experiments at different resolutions, are presented.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesQ. J. R. Meteorol. Soc. - Vol 133
dc.titleAn integrated package for subgrid convection, clouds and precipitation compatible with meso-gamma scales
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freeLocal area modelling
dc.subject.freegrey-zone resolutions
dc.subject.freeprognostic convection
dc.subject.freeprognostic microphysics.
dc.source.issueQ. J. R. Meteorol. Soc. - Vol 133
dc.source.pagep. 711-730
Orfeo.peerreviewedNot pertinent


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