The mathematics of weather and climate Dr Emily Shuckburgh.
Page 1© Crown copyright 2006SRNWP 9-12 October 2006, Zurich Variable resolution or lateral boundary conditions Terry Davies Dynamics Research Yongming.
Antarctic Circumpolar Current
ATMOSPHERIC AND OCEANIC FLUID DYNAMICS
The Quasi-Geostrophic Omega Equation (without friction and diabatic terms) We will now develop the Trenberth (1978)* modification to the QG Omega equation.
The influence of the stratosphere on tropospheric circulation and implications for forecasting Nili Harnik Department of Geophysics and Planetary Sciences,
General Circulation and Kinetic Energy Model output from Warren M. Washington, 1969: .
Shear Instability Viewed as Interaction between Counter-propagating Waves John Methven, University of Reading Eyal Heifetz, Tel Aviv University Brian Hoskins,
Global Convection Modeling (where are we heading and how does this impact HMI?) Mark Miesch HAO/NCAR, JILA/CU (Sacha Brun, Juri Toomre, Matt Browning,
Submesoscale secondary instability in an upwelling system: mechanisms and implications for upper ocean dynamics X. Capet, J. McWilliams, J. Molemaker,
Atms 4320 / 7320 – Lab 7 The Thermal Wind: Forecasting Problems and the Analysis of Fronts.
Q-G Theory: Using the Q-Vector Patrick Market Department of Atmospheric Science University of Missouri-Columbia.
