the atmosphere bulletpoint review for exam. atmosphere: origin 1 st atmosphere: composed of h and...
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Atmosphere: OriginAtmosphere: Origin1st atmosphere: Composed of H
and He. Eroded by solar winds and weak gravity.
Origin Cont.Origin Cont.2nd atmosphere: Composed of gases
released by volcanoes (outgassing). Included all components of current atmosphere except O2 .
Oceans formed from water vapor cooling/condensing.
Origin Fin.Origin Fin.3rd atmosphere: O2 released into
air by splitting of H2O (ozone layer forming @ this time) and primarily by photosynthesis from cyanobacteria. Current O2 at 360 million years ago.
Layers of AtmosphereLayers of Atmosphere5 main layers of atmosphere w/
pseudolayer (ionosphere).
Pressure decreases exponentially w/ alt.
Temp changes vary w/ each specific layer
TroposphereTroposphereClosest to Earth (lowest alt.)
0~15kmClouds, wind, storms, and
precipitation occur in this layer. Tropopause traps H2O
Highest pressure (101KPa, 760mmHg, 1Atm. @ sea level)
Temperature as alt. .
StratosphereStratosphere2nd from ground (15-45km)Ozone layer here.Temp. increases due to O3
molecules absorbing UV rays. From -55˚C to 0 ˚C
Ozone layer shields surface from UV.
MesosphereMesosphereLocated 50-80km alt.Temp. drops rapidly from 0 ˚C to
-80 ˚C (lowest temp. in atmosphere)
ThermosphereThermosphereAbove mesosphere @ 80km-
450kmMain gases are still N2 and O2 but
molecules are up to a kilometer apart (pressure close to vacuum).
Temperature rapidly due to O2 molecules absorbing intense solar radiation.
Temp. climbs to about 980 ˚C.
IonosphereIonosphereNot a layer by location like others,
but rather a location where atm. Gas mol. are ionized by solar radiation.
Radiowaves reflect off e- and allow long range radio comm.
Radios work better @ night since waves travel further into atm. before reflecting.
Organisms and Atm.Organisms and Atm.Plants release O2 into atm. And
animals release CO2. Humans release CFC’s which destroy
O3 mol. and deplete ozone layer.Excess carbon dioxide release by
burning fossil fuels (petroleum, coal, etc.) causes greenhouse effect, trapping solar rays.
Global warming occurs when avg. temp. increase globally.
HumidityHumidityDef: the amount of water in air.Measured by relative hum. which
is amount water/total amount possible
Warm air holds more water since gas mol. further apart, more water mol. can fit.
Dew Point: temp @ which rate condensation and evap. are same.
StratusStratusStratus: lowest to ground layered
and sheetlike.Altostratus: higher alt. stratus.Nimbostratus: stratus clouds w/
rain.
CumulusCumulusCumulus: next lowest to ground.
Fluffy w/ flat bottoms (flat base marks dew point)
Altocumulus: mid alt. cumulus.Cumulonimbus: large rain
bearing cumulus
CirrusCirrusCirrus: high alt. made of
crystalized droplets, have whispy appearance.
Cirrostratus: high layered clouds form veil over sky.
Air PressureAir PressureBarometric pressure/air
pressure/atm. Pressure: the pressure resulting from the weight of air column extending to thermosphere.
Barometer: measures air pressure using mercury pool with a column.
Diff. in pressure cause air to move = Wind.
CoriolisCoriolisEffects the north/south moving
winds by curving them east or west.
Due to rotation of the planet @ diff. velocities depending on latitude.
Weather and ClimateWeather and ClimateAir masses differ in relative
temp.When masses of diff. temp. meet
that is called a front.3 types of front: warm, cold, and
stationary.
Warm FrontWarm FrontWhen warm air mass meets cold
mass.Warm mass slides over top of
cold. This causes cooling, condensing, and precipitation from warm mass.
Preceded by cirrus altostratus and nimbostratus clouds
Cold FrontCold FrontCold mass w/ steep edge lifts
warm mass up.Causes high wind,
thunderstorms, cumulonimbus clouds.
LightningLightningCaused by charge buildup in atm.
by water droplets in clouds as they move.
Spark discharges from ground to sky.
ThunderThunderCaused by rapid (faster than
sound) expansion of air heated by lightning bolt.
The shockwave of superheated air.
TornadoesTornadoesCaused by wind shear b/n cold
dry mass and warm moist mass.
Rotating winds spiraling in opposite directions form upward vortex with highest winds in atm. (500km/hr)
HurricanesHurricanesCaused by tropical depressions
where low pressure gen. by warm water evap. and heating air.
Causes a self feeding system until sufficient strength to form hurricane.
Very large with wind speeds of up to 250km/hr.
ClimateClimateDef: average weather patterns
for a region over many years.
Depends on latitude and variations in topography of land.
Axis Tilt and the SeasonsAxis Tilt and the SeasonsSeasons caused by differences in
amount of direct sunlight due to axis tilt as Earth revolves around sun.
Not dependant on distance to sun. Depends on concentration of solar rays.
Warmer at equator (almost always direct)
Cold at poles (almost always indirect)
Topography and SeasonsTopography and SeasonsDifferent land formations can
affect climate.Mountains force air to increase
alt. causing them to cool, condense, and precipitation. Rainy moist climates leeward.
Rain shadow of mountains due to drier air descending and warming tends to cause desert climates.