Atmospheric Layers

Say Thanks to the AuthorsClick http://www.ck12.org/saythanks

(No sign in required)

To access a customizable version of this book, as well as otherinteractive content, visit www.ck12.org

CK-12 Foundation is a non-profit organization with a mission toreduce the cost of textbook materials for the K-12 market bothin the U.S. and worldwide. Using an open-content, web-basedcollaborative model termed the FlexBook®, CK-12 intends topioneer the generation and distribution of high-quality educationalcontent that will serve both as core text as well as provide anadaptive environment for learning, powered through the FlexBookPlatform®.

Copyright © 2015 CK-12 Foundation, www.ck12.org

The names “CK-12” and “CK12” and associated logos and theterms “FlexBook®” and “FlexBook Platform®” (collectively“CK-12 Marks”) are trademarks and service marks of CK-12Foundation and are protected by federal, state, and internationallaws.

Any form of reproduction of this book in any format or medium,in whole or in sections must include the referral attribution linkhttp://www.ck12.org/saythanks (placed in a visible location) inaddition to the following terms.

Except as otherwise noted, all CK-12 Content (including CK-12Curriculum Material) is made available to Users in accordancewith the Creative Commons Attribution-Non-Commercial 3.0Unported (CC BY-NC 3.0) License (http://creativecommons.org/licenses/by-nc/3.0/), as amended and updated by Creative Com-mons from time to time (the “CC License”), which is incorporatedherein by this reference.

Complete terms can be found at http://www.ck12.org/terms.

Printed: January 8, 2015

www.ck12.org Chapter 1. Atmospheric Layers

CHAPTER 1 Atmospheric Layers

Lesson Objectives

• List the major layers of the atmosphere and their temperatures.• Discuss why all weather takes place in the troposphere.• Discuss how the ozone layer protects the surface from harmful radiation.

Vocabulary

• aurora• exosphere• inversion• ionosphere• magnetosphere• mesosphere• ozone layer• solar wind• stratosphere• temperature gradient• thermosphere• troposphere

Introduction

The atmosphere is layered, corresponding with how the atmosphere’s temperature changes with altitude. By un-derstanding the way temperature changes with altitude, we can learn a lot about how the atmosphere works. Whileweather takes place in the lower atmosphere, interesting things, such as the beautiful aurora, happen higher in theatmosphere.

Air Temperature

Why does warm air rise ( Figure 1.1)? Gas molecules are able to move freely and if they are uncontained, as theyare in the atmosphere, they can take up more or less space.

• When gas molecules are cool, they are sluggish and do not take up as much space. With the same number ofmolecules in less space, both air density and air pressure are higher.

• When gas molecules are warm, they move vigorously and take up more space. Air density and air pressureare lower.

1

www.ck12.org

FIGURE 1.1Papers held up by rising air currents above a radiator demonstrate theimportant principle that warm air rises.

Warmer, lighter air is more buoyant than the cooler air above it, so it rises. The cooler air then sinks down, becauseit is denser than the air beneath it. This is convection, which was described in the Plate Tectonics chapter.

The property that changes most strikingly with altitude is air temperature. Unlike the change in pressure and density,which decrease with altitude, changes in air temperature are not regular. A change in temperature with distance iscalled a temperature gradient.

The atmosphere is divided into layers based on how the temperature in that layer changes with altitude, the layer’stemperature gradient ( Figure 1.2). The temperature gradient of each layer is different. In some layers, temperatureincreases with altitude and in others it decreases. The temperature gradient in each layer is determined by the heatsource of the layer ( Figure 1.3).

FIGURE 1.2The four main layers of the atmospherehave different temperature gradients, cre-ating the thermal structure of the atmo-sphere.

Most of the important processes of the atmosphere take place in the lowest two layers: the troposphere and thestratosphere.

2

www.ck12.org Chapter 1. Atmospheric Layers

FIGURE 1.3The layers of the atmosphere appear asdifferent colors in this image from theInternational Space Station.

Troposphere

The temperature of the troposphere is highest near the surface of the Earth and decreases with altitude. On average,the temperature gradient of the troposphere is 6.5°C per 1,000 m (3.6°F per 1,000 ft.) of altitude. What is the sourceof heat for the troposphere?

Earth’s surface is a major source of heat for the troposphere, although nearly all of that heat comes from the Sun.Rock, soil, and water on Earth absorb the Sun’s light and radiate it back into the atmosphere as heat. The temperatureis also higher near the surface because of the greater density of gases. The higher gravity causes the temperature torise.

Notice that in the troposphere warmer air is beneath cooler air. What do you think the consequence of this is? Thiscondition is unstable. The warm air near the surface rises and cool air higher in the troposphere sinks. So air inthe troposphere does a lot of mixing. This mixing causes the temperature gradient to vary with time and place. Therising and sinking of air in the troposphere means that all of the planet’s weather takes place in the troposphere.

Sometimes there is a temperature inversion, air temperature in the troposphere increases with altitude and warm airsits over cold air. Inversions are very stable and may last for several days or even weeks. Inversions form:

• Over land at night or in winter when the ground is cold. The cold ground cools the air that sits above it, makingthis low layer of air denser than the air above it.

• Near the coast where cold seawater cools the air above it. When that denser air moves inland, it slides beneaththe warmer air over the land.

Since temperature inversions are stable, they often trap pollutants and produce unhealthy air conditions in cities (Figure 1.4).

At the top of the troposphere is a thin layer in which the temperature does not change with height. This means thatthe cooler, denser air of the troposphere is trapped beneath the warmer, less dense air of the stratosphere. Air fromthe troposphere and stratosphere rarely mix.

A science experiment that clearly shows how a temperature inversion traps air, along with whatever pollutants are init, near the ground is seen in this video (5c): http://www.youtube.com/watch?v=LPvn9qhVFbM (2:50).

3

www.ck12.org

FIGURE 1.4Smoke makes a temperature inversionvisible. The smoke is trapped in colddense air that lies beneath a cap ofwarmer air.

MEDIAClick image to the left or use the URL below.URL: http://www.ck12.org/flx/render/embeddedobject/8461

Stratosphere

Ash and gas from a large volcanic eruption may burst into the stratosphere, the layer above the troposphere. Oncein the stratosphere, it remains suspended there for many years because there is so little mixing between the twolayers. Pilots like to fly in the lower portions of the stratosphere because there is little air turbulence.

In the stratosphere, temperature increases with altitude. What is the heat source for the stratosphere? The direct heatsource for the stratosphere is the Sun. Air in the stratosphere is stable because warmer, less dense air sits over cooler,denser air. As a result, there is little mixing of air within the layer.

The ozone layer is found within the stratosphere between 15 to 30 km (9 to 19 miles) altitude. The thickness of theozone layer varies by the season and also by latitude.

The ozone layer is extremely important because ozone gas in the stratosphere absorbs most of the Sun’s harmfulultraviolet (UV) radiation. Because of this, the ozone layer protects life on Earth. High-energy UV light penetratescells and damages DNA, leading to cell death (which we know as a bad sunburn). Organisms on Earth are notadapted to heavy UV exposure, which kills or damages them. Without the ozone layer to reflect UVC and UVBradiation, most complex life on Earth would not survive long ( Figure 1.5).

Mesosphere

Temperatures in the mesosphere decrease with altitude. Because there are few gas molecules in the mesosphere toabsorb the Sun’s radiation, the heat source is the stratosphere below. The mesosphere is extremely cold, especially

4

www.ck12.org Chapter 1. Atmospheric Layers

FIGURE 1.5Even with the ozone layer, UVB radiationstill manages to reach Earth’s surface,especially where solar radiation is high.

at its top, about -90°C (-130°F).

The air in the mesosphere has extremely low density: 99.9% of the mass of the atmosphere is below the mesosphere.As a result, air pressure is very low ( Figure 1.6). A person traveling through the mesosphere would experiencesevere burns from ultraviolet light since the ozone layer which provides UV protection is in the stratosphere below.There would be almost no oxygen for breathing. Stranger yet, an unprotected traveler’s blood would boil at normalbody temperature because the pressure is so low.

Thermosphere and Beyond

The density of molecules is so low in the thermosphere that one gas molecule can go about 1 km before it collideswith another molecule. Since so little energy is transferred, the air feels very cold ( Figure 1.7).

Within the thermosphere is the ionosphere. The ionosphere gets its name from the solar radiation that ionizes gasmolecules to create a positively charged ion and one or more negatively charged electrons. The freed electronstravel within the ionosphere as electric currents. Because of the free ions, the ionosphere has many interestingcharacteristics.

At night, radio waves bounce off the ionosphere and back to Earth. This is why you can often pick up an AM radiostation far from its source at night.

The Van Allen radiation belts are two doughnut-shaped zones of highly charged particles that are located beyond theatmosphere in the magnetosphere. The particles originate in solar flares and fly to Earth on the solar wind. Oncetrapped by Earth’s magnetic field, they follow along the field’s magnetic lines of force. These lines extend from

5

www.ck12.org

FIGURE 1.6Meteors burn in the mesosphere eventhough the gas is very thin; these burningmeteors are shooting stars.

FIGURE 1.7The International Space Station (ISS) or-bits within the upper part of the thermo-sphere, at about 320 to 380 km above theEarth.

above the equator to the North Pole and also to the South Pole then return to the equator.

When massive solar storms cause the Van Allen belts to become overloaded with particles, the result is the mostspectacular feature of the ionosphere – the nighttime aurora ( Figure 1.8). The particles spiral along magnetic fieldlines toward the poles. The charged particles energize oxygen and nitrogen gas molecules, causing them to light up.Each gas emits a particular color of light.

There is no real outer limit to the exosphere, the outermost layer of the atmosphere; the gas molecules finally becomeso scarce that at some point there are no more. Beyond the atmosphere is the solar wind. The solar wind is made of

6

www.ck12.org Chapter 1. Atmospheric Layers

FIGURE 1.8(a) Spectacular light displays are visible as the aurora borealis or northern lights in the Northern Hemisphere. (b)The aurora australis or southern lights encircles Antarctica.

high-speed particles, mostly protons and electrons, traveling rapidly outward from the Sun.

This video is very thorough in its discussion of the layers of the atmosphere. Remember that the chemical composi-tion of each layer is nearly the same except for the ozone layer that is found in the stratosphere (8a): http://www.youtube.com/watch?v=S-YAKZoy1A0 (6:44).

MEDIAClick image to the left or use the URL below.URL: http://www.ck12.org/flx/render/embeddedobject/1600

KQED: Illuminating the Northern Lights

What would Earth’s magnetic field look like if it were painted in colors? It would look like the aurora! This QUESTvideo looks at the aurora, which provides clues about the solar wind, Earth’s magnetic field and Earth’s atmosphere.Learn more at: http://science.kqed.org/quest/video/illuminating-the-northern-lights/ .

MEDIAClick image to the left or use the URL below.URL: http://www.ck12.org/flx/render/embeddedobject/116508

7

www.ck12.org

Lesson Summary

• Features of the atmosphere change with altitude: density decreases, air pressure decreases, temperaturechanges vary.

• Different temperature gradients create different layers within the atmosphere.• The lowest layer is the troposphere where most of the atmospheric gases and all of the planet’s weather are

located. The troposphere is heated from the ground, so temperature decreases with altitude. Because warm airrises and cool air sinks, the troposphere is unstable.

• In the stratosphere, temperature increases with altitude. The stratosphere contains the ozone layer, whichprotects the planet from the Sun’s harmful UV radiation.

Review Questions

1. Give a detailed explanation of why warm air rises.

2. Why doesn’t air temperature change uniformly with altitude? Give examples.

3. Describe how the ground acts as the heat source for the troposphere. What is the source of energy and whathappens to that energy?

4. How stable is an inversion and why? How does an inversion form?

5. Phoenix, Arizona, is a city in the Southwestern desert. Summers are extremely hot. Winter days are often fairlywarm but winter nights can be quite chilly. In December, inversions are quite common. How does an inversion formunder these conditions and what are the consequences of an inversion to this sprawling, car-dependent city?

6. Why can’t air from the troposphere and the stratosphere mix freely?

7. What is the heat source for the stratosphere? How is that heat absorbed?

8. Describe ozone creation and loss in the ozone layer. Does one occur more than the other?

9. How and where are "shooting stars" created?

10. Why would an unprotected traveler’s blood boil in the mesosphere?

Further Reading / Supplemental Links

NASA, The Mystery of the Aurora: http://www.youtube.com/watch?v=PaSFAbATPvk .

Points to Consider

• How does solar energy create the atmosphere’s layers?• How does solar energy create the weather?• What would happen to life on Earth if there was less ozone in the ozone layer?

8

www.ck12.org Chapter 1. Atmospheric Layers

References

1. User:SCEhardt/Wikimedia Commons. http://commons.wikimedia.org/wiki/File:Convection_demo_with_radiator_and_papers.jpg . Public Domain

2. Sam McCabe. CK-12 Foundation . CC BY-NC 3.03. Courtesy of Expedition 23 crew/NASA. http://earthobservatory.nasa.gov/IOTD/view.php?id=44267 . Public

Domain4. Ed Dunens. http://www.flickr.com/photos/blachswan/12476339224/ . CC BY 2.05. Courtesy of NASA. http://earthobservatory.nasa.gov/IOTD/view.php?id=998 . Public Domain6. Courtesy of NASA Ames Research Center/S. Molau and P. Jenniskens. http://commons.wikimedia.org/wik

i/File:Meteor_burst.jpg . Public Domain7. Courtesy of NASA. http://commons.wikimedia.org/wiki/File:ISS_after_STS-120_in_November_2007_1.jpg

. Public Domain8. (a) Courtesy of Senior Airman Joshua Strang, United States Air Force; (b) Courtesy of NASA. (a) hhttp://

commons.wikimedia.org/wiki/File:Polarlicht_2.jpg; (b) http://earthobservatory.nasa.gov/IOTD/view.php?id=6226 . Public Domain

9