11 research outputs found
Documentation of the Fourth Order Band Model
A general circulation model is presented which uses quadratically conservative, fourth order horizontal space differences on an unstaggered grid and second order vertical space differences with a forward-backward or a smooth leap frog time scheme to solve the primitive equations of motion. The dynamic equations for motion, finite difference equations, a discussion of the structure and flow chart of the program code, a program listing, and three relevent papers are given
A stochastic-dynamic model for global atmospheric mass field statistics
A model that yields the spatial correlation structure of atmospheric mass field forecast errors was developed. The model is governed by the potential vorticity equation forced by random noise. Expansion in spherical harmonics and correlation function was computed analytically using the expansion coefficients. The finite difference equivalent was solved using a fast Poisson solver and the correlation function was computed using stratified sampling of the individual realization of F(omega) and hence of phi(omega). A higher order equation for gamma was derived and solved directly in finite differences by two successive applications of the fast Poisson solver. The methods were compared for accuracy and efficiency and the third method was chosen as clearly superior. The results agree well with the latitude dependence of observed atmospheric correlation data. The value of the parameter c sub o which gives the best fit to the data is close to the value expected from dynamical considerations
Multigrid method based on transformation-free high-order scheme for solving 2D Helmholtz equation on nonuniform grids
Untersuchung über die „Boussinesq-Approximation“ bei freier Konvektion in vertikalen porösen Rohren
Modeling Sustainability: Population, Inequality, Consumption, and Bidirectional Coupling of the Earth and Human Systems
Modeling efforts
In this section we survey the historical development of Venus models and the range of models now available, before discussing some of their remaining limitations. We also consider some approaches which have been taken to model Saturn's moon Titan, also a slowly-rotating body with an optically thick, dense atmosphere which super-rotates compared to Titan's surface