1/5
Camille
Thermal Wind Relation
Difference between upper/lower level vectors
Geostrophic Adjustment
Neglect y-direction variation
*PV IS CONSTANT*
Simplifying the QG equation
Rot =1/T < 1 (Rossby), very small number/large time scales
Ro = U/L < 1 (Rossby), weak velocities/large scale flow
Ek= ve/H² < 1 (Ekman number), vertical friction is near 0
QG is a ___ equation
prognostic
Burger Number
Bu = relative vorticity/vertical stretching
NH < fL ← small burger #, vertical stretching dominates
NH > fL ← large burger #, relative vorticity dominates
Available Potential Energy (APE)
the fluid has to correct itself since it is a fixed volume, it is:
existing potential energy - PE of undisturbed fluid