scispace - formally typeset
Open AccessJournal ArticleDOI

The Meso-NH Atmospheric Simulation System. Part I: adiabatic formulation and control simulations

TLDR
The Meso-NH Atmospheric Simulation Engine as mentioned in this paper is a tool for small and meso-scale atmospheric processes, which is based on the Lipps and Hemler form of the anelastic system.
Abstract
The Meso-NH Atmospheric Simulation Sys- tem is a joint eAort of the Centre National de Recher- ches Meteorologiques and Laboratoire d'Aerologie. It comprises several elements; a numerical model able to simulate the atmospheric motions, ranging from the large meso-alpha scale down to the micro-scale, with a comprehensive physical package, a flexible file manager, an ensemble of facilities to prepare initial states, either idealized or interpolated from meteorological analyses or forecasts, a flexible post-processing and graphical facility to visualize the results, and an ensemble of interactive procedures to control these functions. Some of the distinctive features of this ensemble are the following: the model is currently based on the Lipps and Hemler form of the anelastic system, but may evolve towards a more accurate form of the equations system. In the future, it will allow for simultaneous simulation of several scales of motion, by the so-called ''interactive grid-nesting technique''. It allows for the in-line com- putation and accumulation of various terms of the budget of several quantities. It allows for the transport and diAusion of passive scalars, to be coupled with a chemical module. It uses the relatively new Fortran 90 compiler. It is tailored to be easily implemented on any UNIX machine. Meso-NH is designed as a research tool for small and meso-scale atmospheric processes. It is freely accessible to the research community, and we have tried to make it as ''user-friendly'' as possible, and as general as possible, although these two goals sometimes appear contradictory. The present paper presents a general description of the adiabatic formulation and some of the basic validation simulations. A list of the currently available physical parametrizations and ini- tialization methods is also given. A more precise description of these aspects will be provided in a further paper.

read more

Content maybe subject to copyright    Report

Citations
More filters
Dissertation

Paramétrisation des processus physico-chimiques de formation des nuages et étude de leurs impacts sur l'évolution de la composition chimique atmosphérique

TL;DR: Leriche et al. as mentioned in this paper investigated the role of the phase glace and the morphologie des cristaux dans l'evolution chimique du nuage.
Journal ArticleDOI

A Variational Correction Method as an Alternative to Forced Rejection of Sidelobe-Contaminated Bistatic Doppler Measurements

TL;DR: In this article, the authors proposed an alternative solution to the forced rejection of bistatic Doppler data suspected to be contaminated by sidelobe echoes, on the basis of restoring the nonmeasured "actual" (i.e., noncontaminated) BDO velocities from both monostatic radar and Bistatic receiver measurements.

Evapotranspiration partition from the multiple energy balance version of the ISBA-A-gs land surface model over two irrigated crops in a semi-arid Mediterranean region (Marrakech, Morocco)

TL;DR: In this article, the authors compared the performance of the ISBA-A-gs and the multiple energy balance (MEB) version of ISBA using two representations of the canopy energy budget: a coupled 25 approach (ISBA-MEB), where the vegetation layer is located above the soil and a patch representation corresponding to twoadjacent uncoupled source schemes (isBA-2P for 2 patches).
Posted Content

Mixed interpolatory and inference non-intrusive reduced order modeling with application to pollutants dispersion.

TL;DR: This paper proposes a constructive methodology to infer a reduced-order linear, bilinear or quadratic time invariant dynamical model reproducing the underlying phenomena, and shows satisfactory results to predict the pollutants plume pattern while being significantly faster to simulate.

A radar observation operator for high-resolution non-hydrostatic numerical weather prevision

TL;DR: In this paper, a radar simulator was implemented in the research model Meso-NH to specify an observation operator for radar reflectivities for the next numerical weather prediction model of Meteo-France.
References
More filters
Journal ArticleDOI

Fully multidimensional flux-corrected transport algorithms for fluids

TL;DR: In this paper, the critical flux limiting stage is implemented in multidimensions without resort to time splitting, which allows the use of flux-corrected transport (FCT) techniques in multi-dimensional fluid problems for which time splitting would produce unacceptable numerical results.
Journal ArticleDOI

A Simple Parameterization of Land Surface Processes for Meteorological Models

TL;DR: In this article, a parameterization of land surface processes to be included in mesoscale and large-scale meteorological models is presented, where the number of parameters has been reduced as much as possible, while attempting to preserve the representation of the physics which controls the energy and water budgets.
Journal ArticleDOI

A Simple Boundary Condition for Unbounded Hyperbolic Flows

TL;DR: In this article, a Sommerfeld radiation condition (2.2) was proposed for problems requiring a prescribed open boundary, and two severe tests were used to demonstrate the applicability of the open boundary condition: collapsing bubble, a dynamic event which excites many different internal gravity waves.
Book ChapterDOI

Convective parameterization for mesoscale models : The Kain-Fritsch Scheme

TL;DR: The Kain-Fritsch (KF) convective parameterization scheme (CPS) is based on the same fundamental closure assumption as the Fritsch-Chappell (FC) (1980) scheme as mentioned in this paper.
Book ChapterDOI

On the distribution and continuity of water substance in atmospheric circulations

TL;DR: In this paper, the conservation and distribution of water substance in atmospheric circulations are considered within a frame of continuity principles, model air flows, and models of microphysical processes, where the simplest considerations of precipitation involve its vertical distribution in an updraft column, where condensate appears immediately as precipitation with uniform terminal fallspeed.
Related Papers (5)