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9.2: Composition of the Atmosphere

Difficulty Level: At Grade Created by: CK-12
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Did life evolve to match the atmosphere or is the fit just coincidence?

Life as we know it would not survive if there were no ozone layer to protect it from high energy ultraviolet radiation. Most life needs oxygen to survive. Nitrogen is also needed, albeit in a different form from that found in the atmosphere. Greenhouse gases keep the temperature moderate so that organisms can live around the planet. Life evolved to match the conditions that were available and to some extent changed the atmosphere to suit its needs.

Composition of Air

Several properties of the atmosphere change with altitude, but the composition of the natural gases does not. The proportions of gases in the atmosphere are everywhere the same, with one exception. At about 20 km to 40 km above the surface, there is a greater concentration of ozone molecules than in other portions of the atmosphere. This is called the ozone layer .

Nitrogen and Oxygen

Nitrogen and oxygen together make up 99% of the planet’s atmosphere. Nitrogen makes up the bulk of the atmosphere, but is not involved in geological or biological processes in its gaseous form. Nitrogen fixing is described in "Concept Life on Earth." Oxygen is extremely important because it is needed by animals for respiration. The rest of the gases are minor components but sometimes are very important ( Figure below ).

Nitrogen and oxygen make up 99% of the atmosphere; carbon dioxide is a very important minor component.

Water Vapor

Humidity is the amount of water vapor in the air. Humidity varies from place to place and season to season. This fact is obvious if you compare a summer day in Atlanta, Georgia, where humidity is high, with a winter day in Phoenix, Arizona, where humidity is low. When the air is very humid, it feels heavy or sticky. Dry air usually feels more comfortable. When humidity is high, water vapor makes up only about 4% of the atmosphere.

Where around the globe is mean atmospheric water vapor higher and where is it lower ( Figure below )? Why? Higher humidity is found around the equatorial regions because air temperatures are higher and warm air can hold more moisture than cooler air. Of course, humidity is lower near the polar regions because air temperature is lower.

Mean winter atmospheric water vapor in the Northern Hemisphere when temperature and humidity are lower than they would be in summer.

Greenhouse Gases

Remember that greenhouse gases trap heat in the atmosphere. Important natural greenhouse gases include carbon dioxide, methane, water vapor, and ozone. CFCs and some other man-made compounds are also greenhouse gases.

Particulates

Some of what is in the atmosphere is not gas. Particles of dust, soil, fecal matter, metals, salt, smoke, ash, and other solids make up a small percentage of the atmosphere and are called particulates . Particles provide starting points (or nuclei) for water vapor to condense on and form raindrops. Some particles are pollutants.

Summary

  • The major atmospheric gases are nitrogen and oxygen. The atmosphere also contains minor amounts of other gases, including carbon dioxide.
  • Greenhouse gases trap heat in the atmosphere and include carbon dioxide, methane, water vapor, and ozone.
  • Not everything in the atmosphere is gas; particulates are particles that are important as the nucleus of raindrops and snowflakes.

Practice

Use this resource to answer the questions that follow.

http://www.hippocampus.org/Earth%20Science \rightarrow Environmental Science \rightarrow Search: Ozone

1. What is ozone?

2. Where is ozone found?

3. What does ozone do?

4. What does ozone consist of?

5. What does ozone absorb?

Review

1. What are the two major atmospheric gases and what roles do they play?

2. What are the important greenhouse gases?

3. What is humidity?

Vocabulary

humidity

humidity

The amount of water vapor held in the air.
ozone layer

ozone layer

A layer of the stratosphere where ozone gas is more highly concentrated.

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At Grade

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Date Created:

Feb 24, 2012

Last Modified:

Nov 18, 2014
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