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LAYERS OF THE ATMOSPHERE (SCIENCE)
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Earth
is the only planet that is known to
sustain life
in our solar system
One of the factors that make our planet habitable is its
atmosphere
Atmosphere
The
blanket
or envelope of
gases
surrounding the earth
The atmosphere keeps us warm, gives us
oxygen
to breathe, and is where
weather
happens
The
atmosphere
keeps the overall temperature of the earth fairly steady, especially between
night
and day
Gases
in the earth's atmosphere
78%
nitrogen
21%
oxygen
1% other
trace gases
including carbon dioxide, inert gases, hydrogen,
methane
, ozone
Layers
of the atmosphere from ground level upward
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
Basis for dividing the atmosphere into layers
Change of temperature with height
Troposphere
Lowest
layer
Makes up
75
% of total mass of atmosphere
Contains
99
% of atmosphere's water
Where wind, clouds, and weather phenomena take place
Air
is constantly moving
Stratosphere
Air flow is more
stable
than troposphere
Ozone
layer is found here
Protects from
harmful
UV radiation
Mesosphere
Temperature
decreases with height
Coldest
layer
Burns
up most meteors and
asteroids
before reaching Earth's surface
Thermosphere
Closer
to the sun
Absorbs
a large amount of solar radiation
Temperature
increases tremendously
International Space Station and
space shuttles
orbit in this layer
Ionosphere
is found within this layer
Exosphere
Merges into outer space
Temperature varies from very hot to very cold
Ideal for placing artificial satellites as there is little friction
Auroras
are bands of light with different colors, called
aurora borealis
in the north and aurora australis in the south
The stratosphere contains
ozone
, which filters out some
UV radiation
from reaching Earth's surface.
The
troposphere
is the
lowest
layer, where most weather occurs.
The
mesosphere
is the coldest part of the atmosphere, with temperatures dropping to -100°C (-148°F).