Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN system
General yet compact equations are presented to express the thermodynamic impact of physical parameterizations in a NWP or climate model. By expressing the equations in a flux-conservative formulation, the conservation of mass and energy by the physics parameterizations is a built-in feature of the s...
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doaj-4db18cb5d071490f94e9a457da0755be2020-11-24T23:17:15ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032016-06-01962129214210.5194/gmd-9-2129-2016Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN systemD. Degrauwe0Y. Seity1F. Bouyssel2P. Termonia3RMI Belgium, Ringlaan 3, Ukkel, BelgiumCNRM, Météo-France, Avenue Coriolis 42, Toulouse, FranceCNRM, Météo-France, Avenue Coriolis 42, Toulouse, FranceRMI Belgium, Ringlaan 3, Ukkel, BelgiumGeneral yet compact equations are presented to express the thermodynamic impact of physical parameterizations in a NWP or climate model. By expressing the equations in a flux-conservative formulation, the conservation of mass and energy by the physics parameterizations is a built-in feature of the system. Moreover, the centralization of all thermodynamic calculations guarantees a consistent thermodynamical treatment of the different processes. The generality of this physics–dynamics interface is illustrated by applying it in the AROME NWP model. The physics–dynamics interface of this model currently makes some approximations, which typically consist of neglecting some terms in the total energy budget, such as the transport of heat by falling precipitation, or the effect of diffusive moisture transport. Although these terms are usually quite small, omitting them from the energy budget breaks the constraint of energy conservation. The presented set of equations provides the opportunity to get rid of these approximations, in order to arrive at a consistent and energy-conservative model. A verification in an operational setting shows that the impact on monthly-averaged, domain-wide meteorological scores is quite neutral. However, under specific circumstances, the supposedly small terms may turn out not to be entirely negligible. A detailed study of a case with heavy precipitation shows that the heat transport by precipitation contributes to the formation of a region of relatively cold air near the surface, the so-called cold pool. Given the importance of this cold pool mechanism in the life cycle of convective events, it is advisable not to neglect phenomena that may enhance it.http://www.geosci-model-dev.net/9/2129/2016/gmd-9-2129-2016.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
D. Degrauwe Y. Seity F. Bouyssel P. Termonia |
spellingShingle |
D. Degrauwe Y. Seity F. Bouyssel P. Termonia Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN system Geoscientific Model Development |
author_facet |
D. Degrauwe Y. Seity F. Bouyssel P. Termonia |
author_sort |
D. Degrauwe |
title |
Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN system |
title_short |
Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN system |
title_full |
Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN system |
title_fullStr |
Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN system |
title_full_unstemmed |
Generalization and application of the flux-conservative thermodynamic equations in the AROME model of the ALADIN system |
title_sort |
generalization and application of the flux-conservative thermodynamic equations in the arome model of the aladin system |
publisher |
Copernicus Publications |
series |
Geoscientific Model Development |
issn |
1991-959X 1991-9603 |
publishDate |
2016-06-01 |
description |
General yet compact equations are presented to express the thermodynamic
impact of physical parameterizations in a NWP or climate model. By expressing
the equations in a flux-conservative formulation, the conservation of mass
and energy by the physics parameterizations is a built-in feature of the
system. Moreover, the centralization of all thermodynamic calculations
guarantees a consistent thermodynamical treatment of the different processes.
The generality of this physics–dynamics interface is illustrated by applying
it in the AROME NWP model. The physics–dynamics interface of this model
currently makes some approximations, which typically consist of neglecting
some terms in the total energy budget, such as the transport of heat by
falling precipitation, or the effect of diffusive moisture transport.
Although these terms are usually quite small, omitting them from the energy
budget breaks the constraint of energy conservation. The presented set of
equations provides the opportunity to get rid of these approximations, in
order to arrive at a consistent and energy-conservative model. A verification
in an operational setting shows that the impact on monthly-averaged,
domain-wide meteorological scores is quite neutral. However, under specific
circumstances, the supposedly small terms may turn out not to be entirely
negligible. A detailed study of a case with heavy precipitation shows that
the heat transport by precipitation contributes to the formation of a region
of relatively cold air near the surface, the so-called cold pool. Given the
importance of this cold pool mechanism in the life cycle of convective
events, it is advisable not to neglect phenomena that may enhance it. |
url |
http://www.geosci-model-dev.net/9/2129/2016/gmd-9-2129-2016.pdf |
work_keys_str_mv |
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