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atmosphere ch 10

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QuestionAnswer
atmosphere is also made up of solids such as salt, dust, pollen and pollutants
atmosphere a thin layer of air that protects the planet and balances the amount of heat absorbed from the sun with the amount of heat reflected back into space
nitrogen 78% of atmosphere
oxygen 21% of atmosphere
other gases 1%
the atmosphere is also made up of water droplets or vapor 4%
the atmosphere is made up of 5 layers troposphere, stratosphere, mesophere, thermosphere, exophere
troposphere nearest to the earth where all weather happens. has 99% of watervapor and 75% of atmospheric gases. temperature decreases as altitude increases
stratosphere where jets fly. ozone layer, found at the top of stratosphere absorbs UV light and reflect solar energy back into space
mesophere coldest layer, meteors burn, radio waves are reflected to earth, temp decreases with altitude
thermosphere hottest layer, contains the ionsphere where most satellites are, where Aurora Barealis aka Northern Lights happen
ionosphere layer of electrically charged particles within the mesosphere and thermosphere
ionosphere allows radio wavves to travel across the country to another city
exosphere has so few molecules, where the space shuttle orbits Earth
air pressure decreases as you go higher in Earths atmosphere
sun source of most of the energy on Earth
stratosphere temp in this layer rises with increasing altitude
mesosphere temp decreases with altitude
ozone layer located within the stratosphere made of oxygen
ultraviolet radiation energy that comes to Earth from the Sun, too much can damage your skin and cause cancer
chlorofluorocarbons CFCs chemical compounds used in some refrigerators, air conditioners, and aerosol sprays that destroy the ozone
heat is transferred through the atmosphere in three ways radiation, conduction and convection
radiation energy that is transferred in the form of rays or waves and warms your face
conduction is the transfer of energy that occurs when molecules bump into one another
convection third process is the transfer of heat by the flow of material
air is warmed the molecules in it move apart and the air becomes less dense
the equator receives more of the suns energy air near the equator is warmer
warm air is less dense than cold air warm air rises
the poles receive less of the sun's energy air near the poles is colder
cold air is more dense than warm air cold air sinks
warm air molecules are farther apart warm air is less dense
earth rotates the coriolis effect exists
condensation process of water vapor changing to a liquid
westerlies near 30 degrees N and S latitude, moves wind W to E
doldrums along the equator, heating causes air to expand,low pressure, and rainy
trade winds air warmed near the equator travels toward the poles but gradually cools and sinks, coriolis effect, global trade routes.
polar easterlies cold, dense air sinks and moves away from the poles. Wind from E to W
trade winds air descending to Earths surface near 30 degrees N and S latitude creates steady winds that blow in tropical regions
jet streams narrow belts of strong winds
sea breeze movement of air from sea to land
land breeze movement of air toward the water from the land
Created by: leitner6
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