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Layers of the atmosphere

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Presentation on theme: "Layers of the atmosphere"— Presentation transcript:

1 Layers of the atmosphere
Atmosphere- mixture of gases surrounding a planet or moon; air Earth’s Atmospheric Gases: 78% -N 28% - O 1% Ar, Dust, Volcanic ash, sea salt 4 main layers: Troposphere Stratosphere Mesosphere Thermosphere 2 Minor layers: Ionosphere Exosphere

2 Two Special Moms In TN Everyday
Troposphere Stratosphere Mesosphere Ionosphere Thermosphere Exosphere

3 Troposphere Lowest layer we live here only KNOWN layer to support life Tropo means turn most of atmosphere’s weather occurs here Shallowest layer ;but, contains most of the atmosphere’s mass most dense layer Gases mix here As altitude rises temperature decreases

4 Stratosphere layer directly above troposphere Contains O₃- protects us from sun’s uv rays Located km above earth surface Strato means layered or stretching out Gas do not mix here Cold -60⁰C (bottom) to 2,000⁰C at top As altitude increases temperature increases also Air has very little moisture (DRY)

5 Mesosphere Middle layer Coldest layer 50-80 km above Earth’s surface As altitude increases temperature decreases most meteoroids burn up here, producing a meteor trail Protect Earth from meteors Temperature 93⁰ C – 100⁰ C at the top Meteorite- burns up in the Mesos… Meteor- does NOT burn up…hits the Earth

6 Thermosphere Thermo means heat 2,000⁰C at the top Air molecules are 1 km apart N & O convert solar energy to heat Astronauts visit Air very thin: % as dense as the air at sea level Northern lights **even though temperature is hot, thermosphere is NOT hot Heat-transfer of thermal energy Temperature-measure of average energy of particles in motion

7 Ionosphere Located b/t upper mesosphere and lower thermosphere N and O absorb harmful solar energy As temp rises, gases/particles  become electrically charged: ions Auroras-radiated energy seen as shimmering lights in the Polar regions- look this way b/c ions radiate energy AM radio waves can travel around the world here (Frequency) km

8 Exosphere Satellites, Space shuttles Aliens (), Outer space 400 +km- altitude Beyond Cold

9 Formation of wind Sun heats air-causes a rise in temperature-causes a change in air pressure-begins air to moving /convection current=wind Wind is moving air…moves by Convection current Convection current- Transfer of heat by current in a liquid or gas

10 jet streams are narrow belts of high-speed winds that blow in the upper troposphere and lower stratosphere. winds can reach maximum speeds of 400 km/h. Unlike other global winds, the jet streams do not follow regular paths around the Earth.


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