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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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The Advanced Regional Prediction System (ARPS) – A multi-scale nonhydrostatic atmospheric simulation and prediction model. Part I: Model dynamics and verification

TL;DR: The Advanced Regional Prediction System (ARPS) as mentioned in this paper is a non-hydrostatic model developed at the Center for Analysis and Prediction of Storms (CAPS) at the University of Oklahoma.
Journal ArticleDOI

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.
Journal ArticleDOI

A turbulence scheme allowing for mesoscale and large‐eddy simulations

TL;DR: 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.
Journal ArticleDOI

A Global Database of Land Surface Parameters at 1-km Resolution in Meteorological and Climate Models

TL;DR: In this article, the authors presented a new complete surface parameter global dataset at a 1-km resolution, which is intended to initialize the soil-vegetation-atmosphere transfer schemes (SVATs) in meteorological and climate models (at all horizontal scales).
References
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The Multi-Dimensional Crowley Advection Scheme

TL;DR: In this article, the second-order approximation of the first spatial partial derivative is replaced with one that includes information about the dimensionality of the field, and also considering the cross-space difference.
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The Numerical Simulation of Clouds, Rains and Airflow over the Vosges and Black Forest Mountains: A Meso-β Model with Parameterized Microphysics

TL;DR: In this article, a three-dimensional meso-β model with parameterized microphysics is presented, capable of simulating orographically forced clouds, rain, and airflow.
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Journal ArticleDOI

The approach of a vortex pair to a plane surface in inviscid fluid

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