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12.815 Atmospheric Radiation, Fall 2006

Atmospheric radiation blockage.
The dependence of light transmission through the atmosphere on light wavelength. Because of Earth's atmosphere, many wavelengths of radiation cannot be observed by detectors or telescopes on Earth's surface. Only visible light, radio waves, and some ultraviolet light reaches sea level. (Image courtesy of NASA.)

Highlights of this Course

This course features complete lecture notes and computational exercises in assignments section.

Course Description

This is an introduction to the physics of atmospheric radiation and remote sensing including use of computer codes. Subjects covered include: radiative transfer equation including emission and scattering, spectroscopy, Mie theory, and numerical solutions. We examine the solution of inverse problems in remote sensing of atmospheric temperature and composition.
 

Staff

Instructors:
Dr. Robert McClatchey
Prof. Ronald Prinn

Course Meeting Times

Lectures:
One session / week
2 hours / session

Labs:
One session / week
2 hours / session

Level

Graduate

Additional Features

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