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Importance of the Atmosphere
• Earth's atmosphere is a thin layer of air
that forms a protective covering around
the planet.
• Earth's atmosphere maintains a balance
between the amount of heat absorbed from
the Sun and the amount of heat that escapes
back into space.
• It also protects life-forms from some of the
Sun's harmful rays.
1
Earth’s Atmosphere
Makeup of the Atmosphere
• Earth's atmosphere is a mixture of gases,
solids, and liquids that surrounds the planet.
• It extends from Earth's surface to outer space.
1
Earth’s Atmosphere
Makeup of the Atmosphere
• Earth's early atmosphere, produced by
erupting volcanoes, contained nitrogen and
carbon dioxide, but little oxygen.
1
Earth’s Atmosphere
• Then, more than 2
billion years ago,
Earth's early organisms
released oxygen into
the atmosphere as they
made food with the aid
of sunlight.
Makeup of the Atmosphere
• Eventually, a layer rich in ozone (O3) that
protects Earth from the Sun's harmful rays
formed in the upper atmosphere.
• This protective layer eventually allowed
green plants to flourish all over Earth,
releasing even more oxygen.
1
Earth’s Atmosphere
Gases in the Atmosphere
• This circle graph shows the percentages of
the gases, excluding water vapor, that make
up Earth's atmosphere.
1
Earth’s Atmosphere
Gases in the Atmosphere
• The composition of the
atmosphere is changing in
small but important ways.
For example, car exhaust
emits gases into the air.
1
Earth’s Atmosphere
• Humans burn fuel for energy.
• Increasing energy use
may increase the amount
of carbon dioxide in the
atmosphere.
Solids and Liquids in
Earth's Atmosphere
• In addition to gases, Earth's atmosphere
contains small, solid particles such as dust,
salt, and pollen.
1
Earth’s Atmosphere
• The atmosphere also contains small liquid
droplets other than water droplets in clouds.
Solids and Liquids in
Earth's Atmosphere
• The atmosphere constantly moves these
liquid droplets and solids from one region
to another.
1
Earth’s Atmosphere
• For example, the
atmosphere above you
may contain liquid
droplets and solids from
an erupting volcano
thousands of kilometers
from your home.
Layers of the Atmosphere
• Earth’s
atmosphere
has layers.
1
Earth’s Atmosphere
• There are five
layers in Earth’s
atmosphere, each
with its own
properties.
Layers of the Atmosphere
• The lower layers include the troposphere
and stratosphere.
1
Earth’s Atmosphere
• The upper atmospheric layers are the
mesosphere, thermosphere, and exosphere.
• The troposphere and stratosphere contain
most of the air.
Lower Layers of the Atmosphere
• You study, eat, sleep,
and play in the
troposphere, which is
the lowest of Earth’s
atmospheric layers.
1
Earth’s Atmosphere
• It contains 99
percent of the water
vapor and 75
percent of the
atmospheric gases.
Lower Layers of the Atmosphere
• The stratosphere, the layer directly above
the troposphere, extends from 10 km above
Earth's surface to about 50 km.
1
Earth’s Atmosphere
• A portion of the stratosphere contains higher
levels of a gas called ozone.
• Each molecule of ozone is made up of three
oxygen atoms bonded together.
Upper Layers of the Atmosphere
• The mesosphere extends from the top of the
stratosphere to about 85 km above Earth.
1
Earth’s Atmosphere
• The thermosphere is named for its high
temperatures.
• This is the thickest atmospheric layer and
is found between 85 km and 500 km
above Earth.
• The ionosphere
allows radio waves
to travel across the
country to another
city.
• Within the mesosphere and thermosphere is a
layer of electrically charged particles called
the ionosphere (I AH nuh sfihr).
Upper Layers of the Atmosphere
1
Earth’s Atmosphere
Upper Layers of the Atmosphere
• During the day, energy from the Sun interacts
with the particles in the ionosphere, causing
them to absorb AM radio frequencies.
1
Earth’s Atmosphere
• At night, without solar
energy, AM radio
transmissions reflect off
the ionosphere, allowing
radio transmissions to
be received at greater
distances.
Upper Layers of the Atmosphere
• The space shuttle orbits Earth in the exosphere.
1
Earth’s Atmosphere
• The exosphere has so few molecules that the
wings of the shuttle are useless.
• In the exosphere, the
spacecraft relies on
bursts from small
rocket thrusters to
move around.
• Beyond the exosphere
is outer space.
The Ozone Layer
above your head,
lies an atmospheric
layer called the
ozone layer.
• Within the stratosphere, about 19 km to 48 km
1
Earth’s Atmosphere
• Ozone is made of
oxygen.
• Although you cannot
see the ozone layer,
your life depends on it.
The Ozone Layer
• An ozone molecule is made up of
three oxygen atoms bound together.
1
Earth’s Atmosphere
• The ozone layer contains a high
concentration of ozone and shields
you from the Sun's harmful energy.
The Ozone Layer
• Ozone absorbs most of the ultraviolet
radiation that enters the atmosphere.
1
Earth’s Atmosphere
• Ultraviolet radiation is one of the many
types of energy that come to Earth from
the Sun.
CFCs
• Evidence exists that some air pollutants are
destroying the ozone layer.
1
Earth’s Atmosphere
• Blame has fallen on chlorofluorocarbons
(CFCs), chemical compounds used in some
refrigerators, air conditioners, and aerosol
sprays, and in the production of some foam
packaging.
CFCs
• Chlorofluorocarbon molecules destroy ozone.
1
Earth’s Atmosphere
• When a chlorine atom from a
chlorofluorocarbon molecule comes near a
molecule of ozone, the ozone molecule breaks
apart.
• One of the oxygen
atoms combines with
the chlorine atom, and
the rest form a regular,
two-atom molecule.
CFCs
• These compounds don't absorb ultraviolet
radiation the way ozone can.
1
Earth’s Atmosphere
• In addition, the original chlorine atom can
continue to break apart thousands of
ozone molecules.
• The result is that more ultraviolet radiation
reaches Earth's surface.
The Water Cycle
• Hydrosphere is a term that describes all the
water on Earth’s surface.
2
Energy Transfer in the Atmosphere
• The constant cycling of water between the
atmosphere and the hydrosphere plays an
important role in
determining
weather patterns
and climate types.
The Water Cycle
2
Energy Transfer in the Atmosphere

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Atmosphere

  • 1.
  • 2. Importance of the Atmosphere • Earth's atmosphere is a thin layer of air that forms a protective covering around the planet. • Earth's atmosphere maintains a balance between the amount of heat absorbed from the Sun and the amount of heat that escapes back into space. • It also protects life-forms from some of the Sun's harmful rays. 1 Earth’s Atmosphere
  • 3. Makeup of the Atmosphere • Earth's atmosphere is a mixture of gases, solids, and liquids that surrounds the planet. • It extends from Earth's surface to outer space. 1 Earth’s Atmosphere
  • 4. Makeup of the Atmosphere • Earth's early atmosphere, produced by erupting volcanoes, contained nitrogen and carbon dioxide, but little oxygen. 1 Earth’s Atmosphere • Then, more than 2 billion years ago, Earth's early organisms released oxygen into the atmosphere as they made food with the aid of sunlight.
  • 5. Makeup of the Atmosphere • Eventually, a layer rich in ozone (O3) that protects Earth from the Sun's harmful rays formed in the upper atmosphere. • This protective layer eventually allowed green plants to flourish all over Earth, releasing even more oxygen. 1 Earth’s Atmosphere
  • 6. Gases in the Atmosphere • This circle graph shows the percentages of the gases, excluding water vapor, that make up Earth's atmosphere. 1 Earth’s Atmosphere
  • 7. Gases in the Atmosphere • The composition of the atmosphere is changing in small but important ways. For example, car exhaust emits gases into the air. 1 Earth’s Atmosphere • Humans burn fuel for energy. • Increasing energy use may increase the amount of carbon dioxide in the atmosphere.
  • 8. Solids and Liquids in Earth's Atmosphere • In addition to gases, Earth's atmosphere contains small, solid particles such as dust, salt, and pollen. 1 Earth’s Atmosphere • The atmosphere also contains small liquid droplets other than water droplets in clouds.
  • 9. Solids and Liquids in Earth's Atmosphere • The atmosphere constantly moves these liquid droplets and solids from one region to another. 1 Earth’s Atmosphere • For example, the atmosphere above you may contain liquid droplets and solids from an erupting volcano thousands of kilometers from your home.
  • 10. Layers of the Atmosphere • Earth’s atmosphere has layers. 1 Earth’s Atmosphere • There are five layers in Earth’s atmosphere, each with its own properties.
  • 11. Layers of the Atmosphere • The lower layers include the troposphere and stratosphere. 1 Earth’s Atmosphere • The upper atmospheric layers are the mesosphere, thermosphere, and exosphere. • The troposphere and stratosphere contain most of the air.
  • 12. Lower Layers of the Atmosphere • You study, eat, sleep, and play in the troposphere, which is the lowest of Earth’s atmospheric layers. 1 Earth’s Atmosphere • It contains 99 percent of the water vapor and 75 percent of the atmospheric gases.
  • 13. Lower Layers of the Atmosphere • The stratosphere, the layer directly above the troposphere, extends from 10 km above Earth's surface to about 50 km. 1 Earth’s Atmosphere • A portion of the stratosphere contains higher levels of a gas called ozone. • Each molecule of ozone is made up of three oxygen atoms bonded together.
  • 14. Upper Layers of the Atmosphere • The mesosphere extends from the top of the stratosphere to about 85 km above Earth. 1 Earth’s Atmosphere • The thermosphere is named for its high temperatures. • This is the thickest atmospheric layer and is found between 85 km and 500 km above Earth.
  • 15. • The ionosphere allows radio waves to travel across the country to another city. • Within the mesosphere and thermosphere is a layer of electrically charged particles called the ionosphere (I AH nuh sfihr). Upper Layers of the Atmosphere 1 Earth’s Atmosphere
  • 16. Upper Layers of the Atmosphere • During the day, energy from the Sun interacts with the particles in the ionosphere, causing them to absorb AM radio frequencies. 1 Earth’s Atmosphere • At night, without solar energy, AM radio transmissions reflect off the ionosphere, allowing radio transmissions to be received at greater distances.
  • 17. Upper Layers of the Atmosphere • The space shuttle orbits Earth in the exosphere. 1 Earth’s Atmosphere • The exosphere has so few molecules that the wings of the shuttle are useless. • In the exosphere, the spacecraft relies on bursts from small rocket thrusters to move around. • Beyond the exosphere is outer space.
  • 18. The Ozone Layer above your head, lies an atmospheric layer called the ozone layer. • Within the stratosphere, about 19 km to 48 km 1 Earth’s Atmosphere • Ozone is made of oxygen. • Although you cannot see the ozone layer, your life depends on it.
  • 19. The Ozone Layer • An ozone molecule is made up of three oxygen atoms bound together. 1 Earth’s Atmosphere • The ozone layer contains a high concentration of ozone and shields you from the Sun's harmful energy.
  • 20. The Ozone Layer • Ozone absorbs most of the ultraviolet radiation that enters the atmosphere. 1 Earth’s Atmosphere • Ultraviolet radiation is one of the many types of energy that come to Earth from the Sun.
  • 21. CFCs • Evidence exists that some air pollutants are destroying the ozone layer. 1 Earth’s Atmosphere • Blame has fallen on chlorofluorocarbons (CFCs), chemical compounds used in some refrigerators, air conditioners, and aerosol sprays, and in the production of some foam packaging.
  • 22. CFCs • Chlorofluorocarbon molecules destroy ozone. 1 Earth’s Atmosphere • When a chlorine atom from a chlorofluorocarbon molecule comes near a molecule of ozone, the ozone molecule breaks apart. • One of the oxygen atoms combines with the chlorine atom, and the rest form a regular, two-atom molecule.
  • 23. CFCs • These compounds don't absorb ultraviolet radiation the way ozone can. 1 Earth’s Atmosphere • In addition, the original chlorine atom can continue to break apart thousands of ozone molecules. • The result is that more ultraviolet radiation reaches Earth's surface.
  • 24. The Water Cycle • Hydrosphere is a term that describes all the water on Earth’s surface. 2 Energy Transfer in the Atmosphere • The constant cycling of water between the atmosphere and the hydrosphere plays an important role in determining weather patterns and climate types.
  • 25. The Water Cycle 2 Energy Transfer in the Atmosphere