Quasi-Geostrophic Motions in the Equatorial Areas Matsuno (1966) Todd Barron EAS 8802 2 Oct 2007.
Dynamics V: response of the ocean to wind (Langmuir circulation, mixed layer, Ekman layer) L. Talley Fall, 2014 Surface mixed layer - Langmuir circulation.
Thermally-Driven Circulations in Mountain Terrain.
Atms 4320 / 7320 – Lab 7 The Thermal Wind: Forecasting Problems and the Analysis of Fronts.
Chapter 6 Pressure, and the forces that explain the wind.
Q-G Theory: Using the Q-Vector Patrick Market Department of Atmospheric Science University of Missouri-Columbia.
Ch 3 – Pressure, Altitude & Density Introduction Introduction –Pressure and its variations have important applications for aviation, ranging from measurements.
When advection destroys balance, vertical circulations arise COMET-MSC Winter Weather Course 29 Nov. - 10 Dec. 2004 ppt started from one by James T. Moore.
AOSS 401, Fall 2007 Lecture 4 September 12, 2007 Richard B. Rood (Room 2525, SRB) [email protected] 734-647-3530 Derek Posselt (Room 2517D, SRB) [email protected].
The simplifed momentum equations Height coordinatesPressure coordinates.
Thermodynamics, Buoyancy, and Vertical Motion Temperature, Pressure, and Density Buoyancy and Static Stability Adiabatic “Lapse Rates” Dry and Moist Convective.
Announcements Homework Assignment #1 due today. Hand in class or by 5pm to mailbox in PAS building. I will not accept emailed assignments. Groups 3A and.
