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I1: Atmosphere

AB
atmospherea mixture of gases that surrounds a planet or moon
air pressurethe measure of the force which air molecules push on a surface
-sphereball
tropo-turning
strato-layer
meso-middle
thermo-heat
tropospherethe lowest layer of the atmosphere, in which temperature decreases at a constant rate as altitiude increases
stratospherethe layer of the atmosphere that is above the troposphere and in which temperature increases as altitude increases
mesopherethe layer if the atmosphere between the stratosphere and the thermosphere and in which temperature decreases as altitude increases
ozone layerprotects earth by absorbing ultraviolet radiation
thermospherethe uppermost layer of hte atmosphere, in which temperature increases as altitude increases
ionospherealso the thermosphere, because ions are present in the lower part of the thermosphere layer
aurorasin polar regions, the ions radiate energy which cause the lights
radiationthe transfer of energy as electromagnetic waves
thermal conductionthe transfer of energy as heat through a material
convectionthe transfer of thermal energy by the circulation of movement of a liquid of gas
convection currentcycle of warm air rising and cool air sinking causes a circular movement of air
greenhouse effectthe warming of the surface and lower atmosphere of Earth that occurs when water vapor, carbon dioxide, and other gases absorb and reradiate thermal energy
radiation balancethe balance between incoming energy and outgoing energy
global warminga gradual increase in average global temperature
windthe movement of air caused by differences in air pressure
convection cellscircular patterns where air travels
pressure beltsbands of high pressure and low pressure found about 30 degree of latitude
coriolis effectthe curving of the path of winds and ocean currents due to the Earth's rotation
global windsthe combination of convection cells found at every 30 degree of latitude and the Coriolis effect produces patterns of air circulation
polar easterliesprevailing winds that blow from east to west between 60 degrees and 90 degrees latitude in both hemispheres
westerliesprevailing winds that blow west to east between 60 degrees and 90 degrees latitude in both hemispheres
trade windsprevailing winds that blow northeast from 30 degrees north latitude to the equator and that blow southeast from 30 degrees south latitude to the equator
doldrumstrade winds of the northern and southern hemispheres meet in an area around the equator
horse latitudeswinds that that are weak between 30 degrees north and 30 degrees south latitude
jet streamsa narrow belt of strong winds that blow in the the upper troposphere
air pollutionthe contamination of the atmosphere by the introduction of pollutants from the humanand natural sources
primary pollutantspollutants that are put directly into the air by human or natural activity
secondary pollutantspollutants that form when primary pollutants react with other primary pollutants or with naturally occuring substances, such as water vapor
ventilationmixing of indoor air with outdoor air, can reduce indoor air pollution
acid precipitationprecipitation such as rain, sleet, or snow that contains acids from air pollution
acidificationchanges the balance of a soil's chemistry
acid shocka rapid change in a body of water's acidity
scrubbera device that is used to remove some pollutants before they are released by smokestacks


St. James Catholic School
Millstadt, IL

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