Abstract. Long’s equation describes steady-state two-dimensional stratified flow over terrain. Its numerical so-lutions under various approximations were investigated by many authors. Special attention was paid to the properties of the gravity waves that are predicted to be generated as a re-sult. In this paper we derive a time-dependent generalization of this equation and investigate analytically its solutions un-der some simplifications. These results might be useful in the experimental analysis of gravity waves over topography and their impact on atmospheric modeling
Abstract. Internal waves in the atmosphere and ocean are generated frequently from the interaction o...
The case of linear, two-dimensional long waves on a uniform slope is considered. It is assumed that ...
A new 2-D time-dependent model is used to simulate the propagation of an acoustic-gravity wave packe...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain. Its s...
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 which ...
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 two dimensional strat-ified atmospheric flow over terrain which ...
International audienceLong's equation describes two dimensional stratified atmospheric flow over ter...
Long\u27s equation describes two dimensional stratified atmospheric flow over terrain. Its solutions...
Nonlinear analysis of two-dimensional steady flows with density stratification in the presence of gr...
Nonlinear analysis of two-dimensional steady flows with density stratification in the presence of gr...
Previous research regarding the solutions of Long\u27s equation always presumed that the flow far up...
AbstractThe behavior of nonlinear, two-dimensional, transient gravity waves inside an incompressible...
Abstract. Internal waves in the atmosphere and ocean are generated frequently from the interaction o...
The case of linear, two-dimensional long waves on a uniform slope is considered. It is assumed that ...
A new 2-D time-dependent model is used to simulate the propagation of an acoustic-gravity wave packe...
Abstract. Long’s equation describes two dimensional strat-ified atmospheric flow over terrain. Its s...
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 which ...
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 two dimensional strat-ified atmospheric flow over terrain which ...
International audienceLong's equation describes two dimensional stratified atmospheric flow over ter...
Long\u27s equation describes two dimensional stratified atmospheric flow over terrain. Its solutions...
Nonlinear analysis of two-dimensional steady flows with density stratification in the presence of gr...
Nonlinear analysis of two-dimensional steady flows with density stratification in the presence of gr...
Previous research regarding the solutions of Long\u27s equation always presumed that the flow far up...
AbstractThe behavior of nonlinear, two-dimensional, transient gravity waves inside an incompressible...
Abstract. Internal waves in the atmosphere and ocean are generated frequently from the interaction o...
The case of linear, two-dimensional long waves on a uniform slope is considered. It is assumed that ...
A new 2-D time-dependent model is used to simulate the propagation of an acoustic-gravity wave packe...