Time Schedule:
Dale R Durran
ATM S 441
Seattle Campus
Basic equations governing atmospheric motions and their elementary applications; circulation and vorticity; dynamics of midlatitude disturbances. Prerequisite: either AMATH 353 or MATH 309; MATH 324. Offered: A.
Class description
The purpose of the course is to utilize the principles of fluid dynamics to develop an understanding of why large-scale midlatitude weather systems behave as is observed. For example, why do upper-level winds tend to blow parallel to the isobars? Why do troughs, instead of ridges, tend to bring unsettled weather?
Student learning goals
General method of instruction
Recommended preparation
Class assignments and grading