EAE5021 · Advanced dynamical meteorology

Overview

Dynamical meteorology concerns itself with the causes of atmospheric motion. The unit begins with a scale analysis of the equations of motion for mid latitude weather systems, which leads to the most important theoretical development modern meteorology - the quasi-geostrophic theory. This theory and its generalisation, is used to explain Rossby waves and their interaction with the mean state, the development of extratropical cyclones, the causes of vertical motion, and the structure and evolution of cold fronts. The theory for gravity waves is developed also.

Areas of study: Master of Science in Atmospheric Science

Offerings

Assessment

The Handbook lists an examination for this unit.

Assessment details may change. Please refer to the assessment information in Moodle closer to the start of the teaching period.

Requisites

The Handbook lists no prerequisite, corequisite or prohibition for this unit.

Learning outcomes

1. Understand the dynamical principles governing the fluid flow in a rotating frame of reference;
2. Apply these principles to explain the dynamics of many common mid latitude weather systems;
3. Demonstrate a high level of knowledge of the important mathematical techniques used to solve problems in mid latitude dynamics;
4. Read, understand and critically analyse the scientific literature on mid latitude dynamics.

Workload

A total of 12 hours per week comprising: • Twelve 2-hour seminars and • Eight-hours of independent study per week.

Student experience, not official rules. Nothing here changes what the Handbook says.