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Weather

AB
MeteorologistStudies weather
ConductionThe direct transfer of heat energy from one substance to another
convectionThe transfer of heat in a fluid
convection currentsCaused by unequal heating of the atmosphere
radiationtransfer of energy in the form of waves
greenhouse effectGasses forming a "heat blanket"
barometerMeasures air pressure
air pressureVaries according to density
Standard pressureZero degrees Celsius at sea level
windsFormed when air moves from area of high pressure to low
sea breezeFlow of air from sea to land
land breezeFlow of air from land to sea
monsoonA type of seasonal wind
coriolis effectA shift in the path of any object traveling north to south
DoldrumsBelt of warm air around the equator with low pressure
horse latitudesAbout 30 degrees north and south latitude
trade windsWarm air that has dropped and cooled and is heading back to the equator
prevailing westerliesSinking air moving towards the poles
polar easterliesVery cold air flowing towards the equator from the poles
humidityThe amount of water vapor in the air
relative humidityThe amount of water in the air compared to the amount the air can hold
dew pointTemperature at which water vapor turns to liquid
cumulusThis puffy clouds form shapes
cumulonimbusThunderclouds
stratusGray, smooth clouds that cover the entire sky
nimbostratusgray, smooth clouds that produce rain or snow
cirrusVery high, feathery clouds
air massesLarge masses of air with the same consistency through out
maritime tropicalair mass that forms over the ocean near the equator
maritime polarAir mass that forms over the North Pacific and Atlantic
continental polarAir mass that has cold dry air and forms over northern Canada
continental tropicalHot dry air over Mexico and Southern US
frontForms when two air masses meet.
cold frontForms when cold air replaces warm air
warm frontForms when warm air moves over cold air
occluded frontWhen a cold front overtakes a warm front
stationary frontWhen warm air meets cold air and no movement occurs
cycloneArea of low pressure containing rising warm air
anticycloneA high pressure area containing cold dry air
isobarsCurved lines connecting locations that have the same barometric pressure
isothermsCurved lines connecting locations that have teh same temperature
climateThe characteristic of the weather in a region over a long period of time
polar zoneExtends from the pole to about 60 degrees latitude
temperate zoneLocated between 30 and 60 degrees latitude
tropical zoneLocated from 30 degrees latitude to the equator

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