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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.

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Journal ArticleDOI

Gap flow in an Alpine valley during a shallow south föhn event: Observations, numerical simulations and hydraulic analogue

TL;DR: In this article, the authors examined the three-dimensional structure and dynamics of southerly hybrid gap/mountain flow through the Wipp valley (Wipptal), Austria, observed on 30 October 1999 using high-resolution observations and model simulations.
Journal ArticleDOI

Physico-chemical modeling of the First Aerosol Characterization Experiment (ACE 1) Lagrangian B: 1. A moving column approach

TL;DR: In this paper, a one-dimensional Lagrangian boundary layer meteorological model with coupled gas phase photochemistry is used to study the time evolution of gas phases photochemistry in this Lagrangians framework.
Journal ArticleDOI

Synoptic variability of the monsoon flux over West Africa prior to the onset

TL;DR: In this paper, the authors investigated the synoptic variability of the monsoon flux during the establishment of the West African monsoon using observations and ECMWF analyses, highlighting variability at a 3-5-day time scale.
Journal ArticleDOI

Assessment of ForeFire/Meso-NH for wildland fire/atmosphere coupled simulation of the FireFlux experiment

TL;DR: In this paper, a coupled approach between Meso-NH (Non-Hydrostatic) LES (Large Eddy Simulation) mesoscale atmospheric model and ForeFire wildland fire area simulator is compared to experimental data to assess the performance of the proposed coupled approach in predicting fine-scale properties of the dynamics of wildland fires.
Journal ArticleDOI

Benefit of coupling the ISBA land surface model with a TOPMODEL hydrological model version dedicated to Mediterranean flash-floods

TL;DR: In this article, the ISBA land surface model and a version of the TOPMODEL hydrological model have been coupled to simulate Mediterranean flash-floods, making use of the watershed topography to compute the sub-surface lateral water fluxes and spatial and temporal dynamics of the saturated areas.
References
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Journal ArticleDOI

Fully multidimensional flux-corrected transport algorithms for fluids

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Journal ArticleDOI

A Simple Parameterization of Land Surface Processes for Meteorological Models

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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.
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