On the influence of diabatic effects on the motion of 3D-mesoscale vortices within a baroclinic shear flow

3rd M.I.T. Conference on Computational Fluid and Solid Mechanics

Volumn , Issue , 2005, Pages 766-768

  Mikusky, Eileen ^a   Owinoh, Antony Z ^a   Klein, Rupert ^a  

^a POTSDAM INSTITUTE FOR CLIMATE IMPACT RESEARCH   (Germany)

Author keywords

Baroclinic shear flow; Concentrated vortices; Diabatic effects; Matched asymptotic methods

Indexed keywords

ASYMPTOTIC METHOD; BACKGROUND FLOW; BAROCLINIC SHEAR FLOW; CENTERLINES; COHERENT STRUCTURE; COHERENT VORTICES; DIABATIC; HORIZONTAL VELOCITY; MESOSCALE VORTICES; VERTICAL EXTENSION; WIND REGIME;

COMPUTATIONAL FLUID DYNAMICS; ELASTICITY; THREE DIMENSIONAL; VORTEX FLOW;

SHEAR FLOW;

EID: 41249089901     PISSN: None     EISSN: None     Source Type: Conference Proceeding    
DOI: None     Document Type: Conference Paper

References (7)

1. Eady ET. Long Waves and Cyclone Waves, Tellus 1949;1:33-52.
2. Raymond DJ, Jiang H. A theory for long-lived mesoscale convective systems. J Atmos Sci 1990;47:3067-3077.
3. Klein R. An applied mathematical view of meteorological modeling. Proc of ICIAM 2003;227-289.
4. Majda AJ, Klein R. Systematic multi-scale models for the tropics. J Atmos Sci 2000;60:393-408.
5. Kurz M. Leitfäden für die Ausbildung im Deutschen Wetterdienst 8: Synoptische Meteorolgy. Offenbach: Selbstverlag des Deutschen Wetterdienstes, 1990.
6. Callegari A, Ting L. Motion of a curved vortex filament with decaying vortical core and axial velocity. SIAM J Appl Math 1978;35:148-175.
7. Sobel A, Nilsson J, Polvani L. The weak temperature gradient approximation and balanced tropical moisture waves. J Atmos Sci 2001;58:3650-3665.