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Home > Newsevents > Training > Rcourse_notes > NUMERICAL_METHODS > HORIZONTAL_DISCRETIZATION >  
   

Adiabatic formulation of large-scale models of the atmosphere
Finite-difference schemes for the horizontal discretization. April 1994

By A. J. Simmons
European Centre for Medium-Range Weather Forecasts




 
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Table of contents

1 . Introduction

2 . Distribution of grid-points

3 . Staggering of variables
  3.1 Staggered grids
  3.2 The linearized shallow-water equations on an f-plane
  3.2 (a) Discretizations of the linearized shallow-water equations
  3.3 The time-staggered D (Eliassen) grid
  3.4 Grid splitting
  3.5 Applications

4 . Conservation and Eulerian advection schemes
  4.1 Introduction
  4.2 The shallow-water equations on the sphere
  4.3 A conserving finite-difference scheme for the shallow-water equations on the sphere.
  4.4 Some other conserving schemes

5 . Treatment of the poles
  5.1 Formulation of the finite-difference scheme
  5.2 Computational stability

References


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