Physics 61 ‐ Mathematical Methods of Physics.doc

Physics 240
Atmospheric and Environmental Physics
Spring 2006 Syllabus
Instructor: R. David Baker
Moody Science 109
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Class and Laboratory Meeting Time: MWF 1:30-3:00 PM
Office Hours: MWF 3:00-4:00 PM, or by appointment
Course Description
Energy balance at the Earth’s surface and local climate are intricately linked. The Earth system receives most of its energy directly from the Sun. This energy, in the form of ic radiation, is converted to other forms of energy on Earth: infrared radiation, thermal energy, ic energy, and potential energy. Local surface climate conditions influence (and are influenced by) the partitioning of energy into these various forms. For example, deserts may convert most ing solar radiation into thermal and ic energy while oceans may convert most of it into potential energy. Furthermore, energy imbalances help generate storm systems and move mass (such as air or water) from one region to another.
In this project-based course, students will measure the local energy balance at the Austin College Weather Station. Students will be introduced to basic theory of weather, climate, and energy balance. A systems approach will be used in which energy and mass are exchanged between two reservoirs (atmosphere and geosphere). Students will e experts on at least one instrument of the Austin College Weather Station, replace tha