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Introduction
Our atmosphere is comprised by a dynamic mixture of gases that
envelop the earth. Two
gases, nitrogen and oxygen make up most of the atmosphere by volume. They are indeed
important for maintaining life and driving a number of processes near the surface of the
earth. Many of the so called "minor gases" play an equally important role in the
earth system. The minor gases include those that have a significant impact on the heat
budget and the availability of moisture across the earth. The atmosphere is not a
homogeneous mass of gases, but has a layered structure as defined by vertical temperature
changes. In this lecture we'll look at the significance of the major and minor gases and
describe the vertical structure of the earth's atmosphere.
Atmospheric Composition
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Carbon Dioxide - Greenhouse Gas
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Methane - Greenhouse Gas
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Ozone - Absorbs UV; eye and
respiratory irritant; damages plants
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Water vapor Greenhouse
Gas; absorbs long-wave radiation
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Particulates - Absorbs
long-wave or reflects short-wave radiation;
condensation nuclei

Atmospheric Structure
Optional Reading
Optional Audio Program
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describe the significance of the
variable gases to the earth's atmospheric
environment?
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describe characteristics of the troposphere, tropopause, and stratosphere?
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