Atmospheric Chemistry

 Oblique shot of the Earth from space featuring its curvature and atmosphere.

The Earth's atmosphere is showcased in this highly oblique shot of the Earth taken from space. The atmosphere, composed of 78 percent nitrogen, 21 percent oxygen and 1 percent other constituents, shields us from falling meteors, as well as nearly all harmful radiation coming from the sun and other stars. The upper atmosphere also contributes to weather and climate on Earth. (Public domain; Courtesy of NASA/JPL/UCSD/JSC.)

Instructor(s)

MIT Course Number

1.84J / 10.817J / 12.807J

As Taught In

Fall 2013

Level

Graduate

Cite This Course

Course Features

Course Description

This course provides a detailed overview of the chemical transformations that control the abundances of key trace species in the Earth's atmosphere. Emphasizes the effects of human activity on air quality and climate. Topics include photochemistry, kinetics, and thermodynamics important to the chemistry of the atmosphere; stratospheric ozone depletion; oxidation chemistry of the troposphere; photochemical smog; aerosol chemistry; and sources and sinks of greenhouse gases and other climate forcers.

Kroll, Jesse. 1.84J Atmospheric Chemistry, Fall 2013. (MIT OpenCourseWare: Massachusetts Institute of Technology), http://ocw.mit.edu/courses/civil-and-environmental-engineering/1-84j-atmospheric-chemistry-fall-2013 (Accessed). License: Creative Commons BY-NC-SA


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