Monday, October 21, 2019
Free Essays on Earth Sciende
Atmosphere Gas ââ¬â Nitrogen (most abundant), oxygen, / carbon dioxide ââ¬â has the ability to absorb heat radiated by earth, water vapor Atmosphere Pressure is in MB ââ¬â Atmosphere pressure in the PPI ââ¬â Atmosphere pressure at sea level ââ¬â slightly more 1000 millibars, pressure decrease with altitude 3.5 miles 50% atmosphere is below 10 miles 90% atmosphere is below Atmospheric carbon dioxide is transparent to incoming Short-Wavelength solar radiation. But it is not transparent to some of the Long ââ¬âWavelength outgoing terrestrial radiation. Ozone ââ¬âcombines 3 atom oxygen (03) / concentrate between 10-50 kilometers above the stratosphere / absorbs harmful ultraviolet radiation Thermosphere ââ¬â upper limit - Mesosphere ââ¬â temperature decreases - Stratosphere ââ¬â above the troposphere ââ¬â temperature increases at top Troposphere ââ¬â lowermost layer - all important weather phenomena occur - temperature decreases with altitude *** - There is pause in between each Equinoxes ââ¬â occur midway between the solstice - length day equal night - Sept 22-23 march 21-22(spring) Sun angles ââ¬â near water climate = cool summer, warmer winter Northern hemisphere ââ¬â June 21-22 (summer) ââ¬â December 21-22 (winter) Heat transferred in our Earth System -Conduction ââ¬â transfer of heat through matter by molecular activity Convection ââ¬â transfer of heat by the movement of al mass or substance for on place to another Radiation ââ¬â transfer of heat by electromagnetic waves Climate ââ¬â Air Mass ââ¬â Equatorial low ââ¬â rising air ââ¬â abundant precipitation Subtropical high ââ¬â stable - dry air SubPolar low ââ¬â warm and cold winds interact ââ¬â polar front ââ¬â area of storms Polar high ââ¬â cold, subsiding air Leeward side of the mountains ââ¬â usually deficient in moisture Clouds - Cirrus ââ¬â high, white, thin wispy fibers/ Cumulus ââ¬â globular, individual cloud masses/ Stratus ââ¬â sheets or l... Free Essays on Earth Sciende Free Essays on Earth Sciende Atmosphere Gas ââ¬â Nitrogen (most abundant), oxygen, / carbon dioxide ââ¬â has the ability to absorb heat radiated by earth, water vapor Atmosphere Pressure is in MB ââ¬â Atmosphere pressure in the PPI ââ¬â Atmosphere pressure at sea level ââ¬â slightly more 1000 millibars, pressure decrease with altitude 3.5 miles 50% atmosphere is below 10 miles 90% atmosphere is below Atmospheric carbon dioxide is transparent to incoming Short-Wavelength solar radiation. But it is not transparent to some of the Long ââ¬âWavelength outgoing terrestrial radiation. Ozone ââ¬âcombines 3 atom oxygen (03) / concentrate between 10-50 kilometers above the stratosphere / absorbs harmful ultraviolet radiation Thermosphere ââ¬â upper limit - Mesosphere ââ¬â temperature decreases - Stratosphere ââ¬â above the troposphere ââ¬â temperature increases at top Troposphere ââ¬â lowermost layer - all important weather phenomena occur - temperature decreases with altitude *** - There is pause in between each Equinoxes ââ¬â occur midway between the solstice - length day equal night - Sept 22-23 march 21-22(spring) Sun angles ââ¬â near water climate = cool summer, warmer winter Northern hemisphere ââ¬â June 21-22 (summer) ââ¬â December 21-22 (winter) Heat transferred in our Earth System -Conduction ââ¬â transfer of heat through matter by molecular activity Convection ââ¬â transfer of heat by the movement of al mass or substance for on place to another Radiation ââ¬â transfer of heat by electromagnetic waves Climate ââ¬â Air Mass ââ¬â Equatorial low ââ¬â rising air ââ¬â abundant precipitation Subtropical high ââ¬â stable - dry air SubPolar low ââ¬â warm and cold winds interact ââ¬â polar front ââ¬â area of storms Polar high ââ¬â cold, subsiding air Leeward side of the mountains ââ¬â usually deficient in moisture Clouds - Cirrus ââ¬â high, white, thin wispy fibers/ Cumulus ââ¬â globular, individual cloud masses/ Stratus ââ¬â sheets or l...
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