A Fast Numerical Method for Explicit Integration of Primitive Equations Near the Poles,

Abstract

In this paper the three-point method is analyzed and compared to the Fourier method for the numerical solution of the primitive equations in the polar regions. It is shown that the original definition of the latitudinally-dependent parameters of the three-point method results in insufficient frequency reduction compared to the Fourier method. A suitable redefinition of these parameters gives a three-point method that is stable with the time step of the Fourier method, although to prevent the modified frequency from becoming zero in high latitudes requires excessive computation. Consequently the three-point and Fourier methods are combined to form a hybrid method, which is twice as fast as the original Fourier method. An additional doubling of the speed of the hybrid method is achieved by a simple improvement of the Fourier Transform used in the Fourier method. The hybrid method has allowed the time step of the Rand atmospheric GCM to be increased from six to ten minutes with a resultant decrease in time requirement of 37%.

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Document Details

Document Type
Technical Report
Publication Date
Jul 01, 1976
Accession Number
ADA037908

Entities

People

  • Michael E. Schlesinger

Organizations

  • RAND Corporation

Tags

Communities of Interest

  • Air Platforms
  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • California
  • Computational Science
  • Computations
  • Dispersion Relations
  • Equations
  • Fast Fourier Transforms
  • Fluid Dynamics
  • Frequency
  • Gravity
  • Gravity Waves
  • Grids
  • Group Velocity
  • High Latitudes
  • Latitude
  • Rossby Waves
  • Two Dimensional
  • Waves

Readers

  • Approximation Theory.
  • Atmospheric Science/Meteorology