Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain which is represented by the geometry of the domain. The solutions of this equation over simple topography were investigated analytically and numerically by many authors. In this paper we derive a new terrain following formulation of this equation which incorpo-rates the terrain as part of the differential equation rather than the geometry of the domain. This new formulation enables us to compute analytically steady state gravity wave patterns over complex topography in some limiting cases of the pa-rameters that appear in this equation
The continental slope is a region in the ocean that consists of a strong sloping topography. The slo...
In an attempt to understand the dynamical influence of the earth's topography upon the large-scale m...
In numerically integrating the equations of motion in terrain-following coordinates, care must be ta...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain which ...
Long's equation describes two dimensional stratified atmospheric flow over terrain which is rep...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain. Its s...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain. Its s...
Two-dimensional, steady-state, stratified, isothermal atmospheric flow over topography is governed ...
Abstract. Long’s equation describes steady-state two-dimensional stratified flow over terrain. Its n...
Abstract. Internal waves in the atmosphere and ocean are generated frequently from the interaction o...
International audienceLong's equation describes two dimensional stratified atmospheric flow over ter...
AbstractThe behavior of nonlinear, two-dimensional, transient gravity waves inside an incompressible...
Long\u27s equation describes two dimensional stratified atmospheric flow over terrain. Its solutions...
This project examined the theory behind gravity wave analysis and derived methods for detecting the ...
The validity of linear smoothing of topography for numerical weather prediction and the variation of...
The continental slope is a region in the ocean that consists of a strong sloping topography. The slo...
In an attempt to understand the dynamical influence of the earth's topography upon the large-scale m...
In numerically integrating the equations of motion in terrain-following coordinates, care must be ta...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain which ...
Long's equation describes two dimensional stratified atmospheric flow over terrain which is rep...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain. Its s...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain. Its s...
Two-dimensional, steady-state, stratified, isothermal atmospheric flow over topography is governed ...
Abstract. Long’s equation describes steady-state two-dimensional stratified flow over terrain. Its n...
Abstract. Internal waves in the atmosphere and ocean are generated frequently from the interaction o...
International audienceLong's equation describes two dimensional stratified atmospheric flow over ter...
AbstractThe behavior of nonlinear, two-dimensional, transient gravity waves inside an incompressible...
Long\u27s equation describes two dimensional stratified atmospheric flow over terrain. Its solutions...
This project examined the theory behind gravity wave analysis and derived methods for detecting the ...
The validity of linear smoothing of topography for numerical weather prediction and the variation of...
The continental slope is a region in the ocean that consists of a strong sloping topography. The slo...
In an attempt to understand the dynamical influence of the earth's topography upon the large-scale m...
In numerically integrating the equations of motion in terrain-following coordinates, care must be ta...