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Atmosphere CAT 4 Study

AB
Ozoneblocks UV radiuation
High Windfrom steep air pressure gradient
nitrogenmost abundent gas
stable air massno vertical air movement or storms
convergent air flowlow pressure and lifting air
divergent air flowhigh pressure and subsiding air
frontal wedgingwarm air moves up over colder air
orographic liftingair flow move upward when it hits a mountain
Clouds keep the temperaturecooler in the day time and warmer at night
2 most important green house gasesWater vapor and Carbon Dioxide
Ocean currentsmoderate temperature on adjacent land
Increasing elevation causesdecreasing temperature and more precipitation
Tropospherewhere weather happens
relative humidityAmount of water in air / amount of water air can hold
Water in the atmosphere0 - 4%
The cause of global warmingincreased carbon dioxide in air
Carbon Dioxide comes fromburnig fossil fuels, volcanoes, organisms
Water Vapor comes fromevaporation from oceans
greenhouse gasesabsorb Earth's radient enerrgy
Koppen Climate for most of NChumid subtropical
Koppen climateclassifies by temp. and precipitation
Global winds move heatfrom equator toward poles
Solar intensitysun is most intense at equator, less toward poles
occluded frontcold front over takes warm front
Symbol for cold frontline with triangle
symbol for warm frontline with 1/2 circles
symbol for stationary frontline with triangle on one side, and 1/2 circle on the other
eye wallstrongest winds of hurricane
hurricanes on land loose powerfriction and lack of warm water to feed it
Hurricanes formbetween 5 -20 degrees latitude
Hurricane scaleSaffir - Simpson
close isobarshigh winds
winds around high pressureclockwise
winds around low pressurecounterclockwise
El NinoWarm near South America, Dry in Australia and Indonesia
La NinaCold ocean by South America, Wet in Austrailia and Indonesia
Cold frontcold air moves into area where warm air has been
Warm frontwarm air moves into area where clod air has been
Stationary frontcold air and warm air can pass each other with out moving into the other.
maritime polar air masscold and wet air mass
maritime tropical air masswarm and wet air mass
continental polarcold and dry air mass
continental tropicalwarm and dry air mass
which way does air move at high pressuresubsides or descends
which way does air move at low pressuresascends
We like high pressure becausethe weather is clear
Storms usually move across USfrom west to east
West windscome from the west
Air pressure pushesin all directions
Ultimate source of energy for most windssun
isobars are lines thatconnect equal pressure
isotherms are lines thatconnect equal temperature



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