By: Brian C. Bradshaw. Layers of the Atmosphere Exosphere Thermosphere Mesosphere Stratosphere ...
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Transcript of By: Brian C. Bradshaw. Layers of the Atmosphere Exosphere Thermosphere Mesosphere Stratosphere ...
![Page 1: By: Brian C. Bradshaw. Layers of the Atmosphere Exosphere Thermosphere Mesosphere Stratosphere Troposphere Exosphere Thermosphere Mesosphere.](https://reader036.fdocuments.in/reader036/viewer/2022082709/56649d045503460f949d7898/html5/thumbnails/1.jpg)
By: Brian C. BradshawBy: Brian C. Bradshaw
![Page 2: By: Brian C. Bradshaw. Layers of the Atmosphere Exosphere Thermosphere Mesosphere Stratosphere Troposphere Exosphere Thermosphere Mesosphere.](https://reader036.fdocuments.in/reader036/viewer/2022082709/56649d045503460f949d7898/html5/thumbnails/2.jpg)
Layers of the AtmosphereLayers of the Atmosphere
ExosphereThermosphereMesosphereStratosphereTroposphere
ExosphereThermosphereMesosphereStratosphereTroposphere
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TroposphereTroposphere
Starts at earth’s surface and goes 8 to 14.5 kilometers (5-9 miles)
Most dense As you go higher, temperature drops about
17 to 52 degrees Celsius Almost all weather is found in this region Also known as the lower atmosphere
Starts at earth’s surface and goes 8 to 14.5 kilometers (5-9 miles)
Most dense As you go higher, temperature drops about
17 to 52 degrees Celsius Almost all weather is found in this region Also known as the lower atmosphere
![Page 4: By: Brian C. Bradshaw. Layers of the Atmosphere Exosphere Thermosphere Mesosphere Stratosphere Troposphere Exosphere Thermosphere Mesosphere.](https://reader036.fdocuments.in/reader036/viewer/2022082709/56649d045503460f949d7898/html5/thumbnails/4.jpg)
StratosphereStratosphere Starts above troposphere and goes 50
kilometers Dry and less dense than troposphere Temperature increases gradually to -3 degrees
Celsius, due to absorption of ultraviolet radiation
Ozone is in this layer, it absorbs and scatters the solar ultraviolet radiation
99% of “air” is located in the troposphere and stratosphere
Stratopause separates troposphere and stratosphere
Starts above troposphere and goes 50 kilometers
Dry and less dense than troposphere Temperature increases gradually to -3 degrees
Celsius, due to absorption of ultraviolet radiation
Ozone is in this layer, it absorbs and scatters the solar ultraviolet radiation
99% of “air” is located in the troposphere and stratosphere
Stratopause separates troposphere and stratosphere
![Page 5: By: Brian C. Bradshaw. Layers of the Atmosphere Exosphere Thermosphere Mesosphere Stratosphere Troposphere Exosphere Thermosphere Mesosphere.](https://reader036.fdocuments.in/reader036/viewer/2022082709/56649d045503460f949d7898/html5/thumbnails/5.jpg)
MesosphereMesosphere
Starts just above the stratosphere and continues for 85 kilometers (53 miles)
Temperatures fall as low as -93 degrees Celsius as you increase in altitude
Chemicals are in excited state as they absorb energy from the sun
Mesopause separates mesosphere from thermosphere
Stratosphere + Mesosphere = middle atmosphere
Starts just above the stratosphere and continues for 85 kilometers (53 miles)
Temperatures fall as low as -93 degrees Celsius as you increase in altitude
Chemicals are in excited state as they absorb energy from the sun
Mesopause separates mesosphere from thermosphere
Stratosphere + Mesosphere = middle atmosphere
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ThermosphereThermosphere
The thermosphere starts just above the mesosphere and extends to 600 kilometers (372 miles) high.
Temperatures can go as high as 1,727 degrees Celsius.
Chemical reactions occur much faster than on the earth’s surface
Also known as the upper atmosphere
The thermosphere starts just above the mesosphere and extends to 600 kilometers (372 miles) high.
Temperatures can go as high as 1,727 degrees Celsius.
Chemical reactions occur much faster than on the earth’s surface
Also known as the upper atmosphere
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ExosphereExosphere
This is beyond the atmosphere Starts at the top of the thermosphere and
continues until it merges with the interplanetary gases, or space.
In this region of the atmosphere, Hydrogen and Helium are the prime components and are only present at extremely low densities.
This is beyond the atmosphere Starts at the top of the thermosphere and
continues until it merges with the interplanetary gases, or space.
In this region of the atmosphere, Hydrogen and Helium are the prime components and are only present at extremely low densities.