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A turbulence scheme allowing for mesoscale and large‐eddy simulations

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In this paper, the authors describe the turbulence scheme implemented in the Meso-NH community research model, and report on some validation studies, and compare the results of three idealized boundary-layer simulations allowing detailed comparisons with other large-eddy simulation (LES) models.
Abstract
The paper describes the turbulence scheme implemented in the Meso-NH community research model, and reports on some validation studies. Since the model is intended to perform both large-eddy and mesoscale simulations, we have developed a full three-dimensional scheme, based on the original method of Redelsperger and Sommeria. A prognostic equation for the turbulent kinetic energy is used, together with conservative variables for moist non-precipitating processes. A particularity of the scheme is the use of variable turbulent Prandtl and Schmidt numbers, consistently derived from the complete set of second-order turbulent-moment equations. The results of three idealized boundary-layer simulations allowing detailed comparisons with other large-eddy simulation (LES) models are discussed, and lead to the conclusion that the model is performing satisfactorily. The vertical flux and gradient computation can be run in isolation from the rest of the scheme, providing an efficient single-column parametrization for the mesoscale configuration of the model, if an appropriate parametrization of the eddy length-scale is used. The mixing-length specification is then the only aspect of the scheme which differs from the LES to the mesoscale configuration, and the numerical constants used for the closure terms are the same in both configurations. The scheme is run in single-column mode for the same three cases as above, and a comparison of single-column and LES results again leads to satisfactory results. It is believed that this result is original, and is due to the proper formulation of the parametrized mixing length and of the turbulent Prandtl and Schmidt numbers. In fact, a comparison of the parametrized mixing length with the length-scale of the energy-containing eddies deduced by spectral analysis of the LES shows interesting similarity.

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The AROME-France Convective-Scale Operational Model

TL;DR: The application of research to operations at Mesoscale (AROME-France) convective-scale model became operational at Meteo-France at the end of 2008 as mentioned in this paper, and the main characteristics of this new numerical weather prediction system: the nonhydrostatic dynamical model core, detailed moist physics, and the as- sociated three-dimensional variational data assimilation (3D-Var) scheme.
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The Rossby Centre Regional Climate model RCA3: model description and performance

TL;DR: The Rossby Centre Regional Climate Model (RCA3) as mentioned in this paper is the most recent version of the RCA3 model and is based on a tiled land-surface scheme.
References
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General circulation experiments with the primitive equations

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Development of a turbulence closure model for geophysical fluid problems

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A Hierarchy of Turbulence Closure Models for Planetary Boundary Layers.

TL;DR: In this article, the authors consider simplification based on the observation that the parameters governing the degree of anisotropy are small, and propose a simplification approach for the problem of a planetary boundary layer subject to a diurnally varying surface heat flux or surface temperature.
Journal ArticleDOI

A parametric model of vertical eddy fluxes in the atmosphere

TL;DR: In this paper, a model for the representation of vertical eddy fluxes of heat, momentum and water vapour in a forecast model is presented, and two tests are presented, using the scheme in a one-dimensional model: the simulation of the diurnal cycle and the transformation of a polar air mass moving over the warm sea.
Journal ArticleDOI

Stratocumulus-capped mixed layers derived from a three-dimensional model

TL;DR: In this article, a three-dimensional numerical model was used to study turbulence and entrainment within mixed layers containing stratocumulus with or without parameterized cloud-top radiative cooling.
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