230 likes | 330 Views
The Atmosphere. THE ATMOSPHERE. Definition: Atmosphere. Air that surrounds the earth Composed of: Nitrogen 78% Oxygen 21% Misc. Gases (water vapor, argon, etc… 1%). How did it form?. THEORY ………. As earth cooled, released gases from the earth’s interior
E N D
The Atmosphere THE ATMOSPHERE
Definition: Atmosphere • Air that surrounds the earth • Composed of: • Nitrogen 78% • Oxygen 21% • Misc. Gases (water vapor, argon, etc… 1%)
How did it form? • THEORY ………. • As earth cooled, released gases from the earth’s interior • Not the same composition as today’s atmosphere
Benefits of Atmosphere • Provides gases necessary for life (oxygen, carbon dioxide) • Protects us from majority of suns harmful UV radiation • Allows light to reach surface for energy and photosynthesis • Radiates some heat back to Earth, therefore warming the planet
Layers • Defined by changes in temperature • Troposphere • tropopause • Stratosphere • stratopause • Mesosphere • mesopause • Thermosphere
Troposphere • 0-12 km • Where we live • Weather occurs here • As height increases, temperature decreases • Temperature drops ~ 6.50 C/km above Earth’s surface • Greatest amount of air pressure (weight of air above)
Tropopause • Top of troposphere • Temperature fairly constant • Separates troposphere from stratosphere • Where jet stream is • Very strong winds that blow eastward
Stratosphere • 12 – 50 km • Lower part’s temperature is constant (~60oC) • Contains ozone layer • People can’t breathe in this layer • Lowest part of stratosphere there is less turbulence so where commercial airlines usually fly!
Ozone Layer • Earth’s shield • Protects Earth’s surface from the sun’s harmful UV radiation • It absorbs the sun’s UV radiation • Causes an increase in temperature in upper part of stratosphere
Mesosphere • 50 – 80 km • Temperature decrease to -100oC • Coldest region of atmosphere • This is due to the gases in this layer can’t absorb any of the suns energy (therefore, really cold) • Protects earth from ‘meteorites’ • Meteorites burn up in this area creating “shooting stars” effect
Thermosphere • 80 km and up • Air very thin • Temperaturesvery high because of sun’s intense UV radiation • Temps can be >2000oC • Has 2 sub-layers • Ionoshpere • exosphere
Ionosphere • 80 km – 550 km • Contains charged “ionic” particles • Where radio waves are bounced back from
Exosphere • > 550 km. • Air extremely thin • Area where satellites orbit • Enter space once exit exosphere
Magnetosphere • Earth’s magnetic field • Causes Northern Lights
Assignment • Create a foldable of the layers of the atmosphere. • READ AND FOLLOW THE DIRECTIONS !!!! DO THIS STEP BY STEP !