Geography 101 The Physical Environment
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Atmospheric Structure and
Composition

 

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

Permanent Gases (% by volume)

  • Nitrogen 78

  • Oxygen 21

Variable Gases (% by volume)

  • Carbon Dioxide - Greenhouse Gas 

  • Methane - Greenhouse Gas

  • Ozone - Absorbs UV; eye and respiratory irritant; damages plants

  • Water vapor  Greenhouse Gas; absorbs long-wave radiation

  • Particulates - Absorbs long-wave or reflects short-wave radiation; condensation nuclei


 

 

Atmospheric Structure

  • Atmosphere subdivided on the basis of temperature change

Troposphere

Tropopause

Stratosphere

 


Optional Reading

Optional Audio Program

  • "Ozone Layer" Listen to this NPR segment from May 2000 about the ozone hole over the Arctic.



world_question_mark.GIF (5415 bytes)Can you....

  • describe the significance of the variable gases to the earth's atmospheric environment?

  • describe characteristics of the troposphere, tropopause, and stratosphere?


 

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© Michael Ritter mritter@uwsp.edu
Last revised March 11, 2007