ch17 atmosphere

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Created by:

lindseyeichelman  on January 15, 2011

Subjects:

science

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ch17 atmosphere

weather
the state of the atmosphere at any given time and place
mostly nitrogen and oxygen
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weather the state of the atmosphere at any given time and place
mostly nitrogen and oxygen
the source of all clouds water
why is the ozone layer crucial to life on earth it absorbs harmful uv rays from the sun.
without it earth would be uninhabitable for many organisms
troposphere temperature decreases with increase in altitude
all important weather phenomena occur here
thickness varies with latitude and season
temperature drop continues to about 12km
stratosphere temperature remains constant to a heigh of 20km the begins to gradually increase because the atmospheres ozone absorbs hot uv rays
mesosphere temperature decreases until mesopause
thermosphere has no well defined limit
temperature increases because of sun
oxygen and nitrogen absorb shortwave, high energy solar radiation
radiation transfer of heat through space by electromagnetic waves
travels out in all directions from source
can travel through the vacuum of space/no material needed
convection transfer of heat by mass movement or circulation within a substance
atoms and molecules are free to move about
median-fluids=oceans and air
solids=earths matels
conduction the transfer of hear through matter by molecular activity
energy of molecules by collisions from once molecule to another
median=metals
rotation spinning causing day and night
revolution earth going around the sun creating years
what causes seasons tilt of the earth
how much does the earth tilt 23.5 degrees
solstice describes when the tilt of the earths axis is realtive to the sun at the maximum -23.5 degrees
equinox no tilt od the earths axis relative to the sun
12 hours of light and night
why does only about half of incoming solar radiation reach the surface scattering and reflecting off clouds/atmosphere
isotherms lines that connect points that have the same temperature
albedo percent of solar radiation reflected by a surface
factors that exert a strong influence on temperature latitude
heating of land and water
altitude
geographic position
cloud cover
ocean currents
greenhouse effect the heating of earths surface and atmosphere from solar radiation being absorbed and emitted by the atmosphere
maint by water vapor and carbon dioxide

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