Q-G vorticity equation Q-G thermodynamic equation We now have two equations in two unknowns, and We will solve these to find an equation for , the.
Surface winds An air parcel initially at rest will move from high pressure to low pressure (pressure gradient force) Geostrophic wind blows parallel to.
Vorticity. The Law of conservation of Vorticity Relative vorticity is defined as The time rate of change of vorticity can be written by taking the equations.
Ocean & Atmospheric circulation redux 1) Unequal planetary heating creates pressure gradients which make winds blow on ocean surface in trade-wind & westerly.
Modeling Deep Convective Zonal Flows on the Giant Planets Jonathan Aurnou UCLA Earth & Space Sciences [email protected] Cassini Image.
Ocean & Atmospheric circulation redux
Tropical Cyclone Energy Dispersion in a Three-Dimensional Primitive Equation Model: Upper-Tropospheric Influence Ge X., T. Li, Y. Wang, and M. S. Peng,
AOSS 401, Fall 2006 Lecture 19 October 26 , 2007
Intrinsic Errors in Physical Ocean Climate Models Matthew Hecht Los Alamos National Laboratory.
Modeling Deep Convective Zonal Flows on the Giant Planets
Complex 2D Fields: Analysis of Eddies in the Southern Indian Ocean
AOSS 401, Fall 2006 Lecture 19 October 26, 2007 Richard B. Rood (Room 2525, SRB) [email protected] 734-647-3530 Derek Posselt (Room 2517D, SRB) [email protected].
