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Ava Sawyer - Humans and Earths Atmosphere: Whats in the Air?

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Ava Sawyer Humans and Earths Atmosphere: Whats in the Air?
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Nitrogen, oxygen, argon, and carbon dioxide are all gases in Earths atmosphere. But what happens when there is too much or two little of a certain gas? Readers will learn how every day activities such as driving, heating buildings, and using aerosols release harmful gases into the air and how it affects the air we breathe. Meets Next Generation Science Standards.

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CHAPTER 1 WHAT IS THE ATMOSPHERE Earths atmosphere is a blanket of gases that - photo 1
CHAPTER 1 WHAT IS THE ATMOSPHERE Earths atmosphere is a blanket of gases that - photo 2
CHAPTER 1
WHAT IS THE ATMOSPHERE?

Earths atmosphere is a blanket of gases that surrounds the planet. From space, our atmosphere looks like a thin blue band of air. The atmosphere has several purposes. It gives plants and animals the carbon dioxide and oxygen they need to survive. The atmosphere protects the planet by acting like a shield, blocking harmful asteroids from outer space. It also helps to control the amount of the suns energy that reaches Earths surface. The gases in the atmosphere help to moderate Earths temperature. They keep it from becoming too hot or too cold for life on Earth.

Sunlight reflects off of Earths atmosphere Earths atmosphere is made up of 78 - photo 3

Sunlight reflects off of Earths atmosphere.

Earths atmosphere is made up of 78 percent nitrogen, 21 percent oxygen, 0.93 percent argon, and 0.038 percent carbon dioxide. Water vapor is also a part of the atmosphere. It varies between 0 and 4 percent of the atmosphere. The amount of water vapor depends upon the location on Earth, time of day, time of year, and current weather conditions. Earths atmosphere isnt the same all the way through. The atmosphere is divided into five separate layers. Beginning with the layer closest to the earth and moving outward is the .

The troposphere layer is closest to Earths surface The exosphere layer fades - photo 4

The troposphere layer is closest to Earths surface. The exosphere layer fades into outer space.

TROPOSPHERE

The troposphere is the layer of the atmosphere closest to Earth. It begins at Earths surface and goes upward between 0 and 7 miles (0 and 11 km). The troposphere is the densest part of the entire atmosphere. It is densest at Earths surface. The very top of the troposphere is called the tropopause.

The troposphere gets thinner as you move up in the layer Thats why Mount - photo 5

The troposphere gets thinner as you move up in the layer. Thats why Mount Everest climbers need to bring oxygen tanks with them.

STRATOSPHERE

The stratosphere begins just above the tropopause. The highest point of the stratosphere layer stretches 31 miles (50 km) above Earth. In the troposphere, temperature decreases with altitude. The higher you go, the colder it gets.

THE OZONE LAYER

One of the layers in the stratosphere is the ultraviolet radiation. When the ozone layer is destroyed, more harmful radiation makes its way to Earth.

Chlorofluorocarbons

One problem of the stratosphere is that any particle that ends up in this layer can stay there for a long time for months or even years. Ozone-destroying chemicals like chlorofluorocarbons are one concern in the stratosphere. Chlorofluorocarbons (CFCs) are chemicals that contain atoms of carbon, chlorine, and fluorine. They are used in the manufacturing of aerosol sprays and can destroy stratospheric ozone.

MESOSPHERE

The mesosphere stretches from about 31 miles (50 km) above Earth to 50 miles (80 km) above Earth. Less is known about the mesosphere than any of the other layers. Its difficult for scientists to study this layer. Its too high for weather balloons and aircraft to fly, and its too low for satellites.

NASA launches a suborbital sounding rocket carrying student experiments on June - photo 6

NASA launches a suborbital sounding rocket carrying student experiments on June 26, 2015.

FACT

To learn more about this layer, scientists from NASA send sounding rockets into the mesosphere. These rockets carry scientific instruments into space. These missions only last between 5 and 20 minutes. During that time scientists are able to obtain new data about this area of the atmosphere.

THERMOSPHERE

This layer of the atmosphere has very hot temperatures. The gases in this layer absorb high-energy radiation, causing extremely high temperatures in the thermosphere. The main parts of air in the upper thermosphere include oxygen atoms, nitrogen atoms, and helium.

EXOSPHERE

The highest part of the atmosphere is called the exosphere. There isnt a distinct line between Earths atmosphere and outer space. The atmosphere eventually gets so thin that it becomes an empty vacuum of space. Some scientists argue that outer space starts much lower in the thermosphere. Others think outer space begins at the edge of the exosphere. They say that atmosphere is still present until the lightest particles, such as hydrogen atoms, start escaping from Earths gravity and into space. The exosphere is composed almost entirely of hydrogen gas. There are only small amounts of other atmospheric gases like oxygen, helium, and carbon dioxide.

The word exosphere comes from the Greek word exo which means outside and - photo 7

The word exosphere comes from the Greek word exo , which means outside, and sphaira , which means sphere.

CHAPTER 2
THE INDUSTRIAL REVOLUTION

In the modern era, humans have made a big impact on the atmosphere. Humans began burning materials formed from plants and animals that died millions of years ago. Newly invented machines during this time needed energy to run. This energy came from the burning of the fossil fuel coal. Soon, coal smoke filled the sky. Some cities were so polluted it looked like nighttime in the middle of the day.

A fossil fuel power plant releases smoke into the air while operating These - photo 8

A fossil fuel power plant releases smoke into the air while operating.

These types of conditions remained in some cities into the mid-1900s. They are still present in places that lack air pollution regulations. The city of Beijing, China, for example, is highly polluted. The majority of homes and power plants still burn coal. When conditions are really severe in Beijing, people have to wear masks. They also have to limit outdoor activities as much as possible.

Air pollution fills the air in Beijing China in 2015 In the beginning of the - photo 9

Air pollution fills the air in Beijing, China, in 2015.

In the beginning of the Industrial Revolution, some factory owners thought it didnt matter how much smoke they put into the air. Over time, though, humans have learned how dangerous it is to treat the atmosphere this way.

CHAPTER 3
FOSSIL FUELS

Fossil fuels formed from dead plants and animals. Their bodies were buried in the earth. Other layers piled on top. Great pressure caused the organic materials to turn to rock. Some of this organic material became coal. Living things are made up of carbon, so fossil fuels also have carbon. When fossil fuels are burned, carbon turns into carbon dioxide. Then it is released into the atmosphere.

Coal is combustible meaning it burns easily Carbon dioxide is a fossil fuels - photo 10
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