|
|
|
|
|
Ismael Pérez-García,Alejandro Aguilar-Sierra,Jaime Steven Hernández-Alfaro
Pág. 285 - 300
Tropical cyclone Mitch, which occurred in October 1998 on the Caribbean Sea, is studied. Mitch affected countries in Central America, where it caused great economic and human losses, and the authors believe that the scientific community has not paid enou...
ver más
|
|
|
|
|
|
|
|
|
|
|
Ismael Pérez-García
Pág. 179 - 190
The purpose of this paper is to represent the exact solutions of the barotropic vorticity equations (BVE) on the rotating unit sphere S2 as a manifold, which are zonal flows, Rossby-Haurwitz waves and generalized solutions named modons. Modern methods of...
ver más
|
|
|
|
|
|
|
|
|
|
|
Yuri N. Skiba
Pág. 283 - 296
The nonlinear barotropic vorticity equation (BVE) describing the vortex dynamics of viscous incompressible and forced fluid on a rotating sphere is considered. The asymptotic behavior of solutions of nonstationary BVE as t ? 8 is studied. Particular form...
ver más
|
|
|
|
|
|
|
|
|
|
|
E. E. VILLANUEVA,V. MANUEL MENDOZA,JULIAN ADEM
Numerical solutions of the barotropic vorticity equation under forcing by wind stress, and mass transport between the basins of the Caribbean Sea and the Gulf of Mexico, are shown, in the first part of this study, the equation was solved for a stea...
ver más
|
|
|
|
|
|
|
|
|
|
|
ISMAEL PÉREZ GARCÍA,YURI N. SKIBA
A numerical algorithm for the normal mode instability study of a steady nondivergent flow on a rotating sphere is developed. The algorithm accuracy is tested with zonal solutions of the nonlinear barotropic vorticity equation (Legendre polynomials, zo...
ver más
|
|
|
|
|
|
|
|
|
|
|
ISMAEL PÉREZ GARCÍA,YURI N. SKIBA
A numerical spectral model of the barotropic atmosphere is used to simulate well-known exact solutions of the vorticity equation for an ideal incompressible fluid on a rotating sphere. Primary emphasis is received to the behavior of the relative error...
ver más
|
|
|
|
|
|
|
|
|
|
|
A. WIIN NIELSEN
A simple low-order nonlinear model with forcing and dissipation is used to demonstrate that inter-monthly oscillations may be caused by the nonlinear interaction. The length of the period depends on the intensity of the forcing. The model used for the...
ver más
|
|
|
|
|
|