Mathematical Research Data Initiative
Main page
Recent changes
Random page
Help about MediaWiki
Create a new Item
Create a new Property
Create a new EntitySchema
Merge two items
In other projects
Discussion
View source
View history
Purge
English
Log in

Scale-dependent merging of baroclinic vortices

From MaRDI portal
Publication:4304644
Jump to:navigation, search

DOI10.1017/S0022112094000595zbMath0800.76514MaRDI QIDQ4304644

S. Valcke, Jacques Verron

Publication date: 31 August 1994

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)



Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Vortex flows for incompressible inviscid fluids (76B47) Reaction effects in flows (76V05)


Related Items (4)

Formation of small-scale vortices in the core of a large merged vortex ⋮ The stability and the nonlinear evolution of quasi-geostrophic hetons ⋮ Coalescence of lenticular anticyclones in a linearly stratified rotating fluid ⋮ Vortex merger near a topographic slope in a homogeneous rotating fluid



Cites Work

  • Two-layer geostrophic vortex dynamics. Part 2. Alignment and two-layer V-states
  • Symmetric vortex merger in two dimensions: causes and conditions
  • Evolution and merger of isolated vortex structures
  • The emergence of isolated coherent vortices in turbulent flow
  • Contour dynamics for the Euler equations in two dimensions


This page was built for publication: Scale-dependent merging of baroclinic vortices

Retrieved from "https://portal.mardi4nfdi.de/w/index.php?title=Publication:4304644&oldid=18242410"
Tools
What links here
Related changes
Special pages
Printable version
Permanent link
Page information
MaRDI portal item
This page was last edited on 6 February 2024, at 20:41.
Privacy policy
About MaRDI portal
Disclaimers
Imprint
Powered by MediaWiki