The planetary background rotation and density stratification play an essential role in the dynamics of most large-scale geophysical vortices. In this chapter we will discuss some basic dynamical aspects of rotation and stratification, while focusing on elementary vortex structures. Rotation effects will be discussed in Sect. 1.1, attention being given to basic balances, Ekman-layer effects, topography and ß-plane effects, and vortex instability. Some laboratory experiments will be discussed in order to illustrate the theoretical issues. Section 1.2 is devoted to vortex structures in stratified fluids, with focus on theoretical models describing their decay. Again, laboratory experiments will play a central part in the discussion. Finally, s...
In linear stratifications, vortices have a typical flat shape that appears to be not only ...
Turbulence is ubiquitous within geophysical and astrophysical fluid flows. Its interaction with phys...
We present the results of an experimental investigation of the generation of coherent vortical struc...
The planetary background rotation and density stratification play an essential role in the dynamics ...
This book presents an extensive analysis of the dynamics of discrete and distributed baroclinic vort...
Investigators have modeled oceanic and atmospheric vortices in the laboratory in a number of differe...
The contents of the book cover topics on vortex dynamics in a variety of flow problems and describe ...
International audienceIn inviscid fluids with uniform density, it is common to idealize three-dimens...
The dynamics and the three-dimensional structure of vortices in a linearly stratified, non-rotating ...
Large coherent vortices are abundant in geophysical and astrophysical flows. They play significant r...
International audienceThe dynamics of a baroclinic vortex in a two-layer rotating stratified fluid i...
This paper reviews some aspects of topography effects on the dynamics of barotropic monopolar, dipol...
The key element of Geophysical Fluid Dynamics—reorganization of potential vorticity (PV) by nonlinea...
L’océan et l’atmosphère sont des environnements fluides stratifiés en densité, en référentiel tourna...
In linear stratifications, vortices have a typical flat shape that appears to be not only ...
Turbulence is ubiquitous within geophysical and astrophysical fluid flows. Its interaction with phys...
We present the results of an experimental investigation of the generation of coherent vortical struc...
The planetary background rotation and density stratification play an essential role in the dynamics ...
This book presents an extensive analysis of the dynamics of discrete and distributed baroclinic vort...
Investigators have modeled oceanic and atmospheric vortices in the laboratory in a number of differe...
The contents of the book cover topics on vortex dynamics in a variety of flow problems and describe ...
International audienceIn inviscid fluids with uniform density, it is common to idealize three-dimens...
The dynamics and the three-dimensional structure of vortices in a linearly stratified, non-rotating ...
Large coherent vortices are abundant in geophysical and astrophysical flows. They play significant r...
International audienceThe dynamics of a baroclinic vortex in a two-layer rotating stratified fluid i...
This paper reviews some aspects of topography effects on the dynamics of barotropic monopolar, dipol...
The key element of Geophysical Fluid Dynamics—reorganization of potential vorticity (PV) by nonlinea...
L’océan et l’atmosphère sont des environnements fluides stratifiés en densité, en référentiel tourna...
In linear stratifications, vortices have a typical flat shape that appears to be not only ...
Turbulence is ubiquitous within geophysical and astrophysical fluid flows. Its interaction with phys...
We present the results of an experimental investigation of the generation of coherent vortical struc...