Java Games: Flashcards, matching, concentration, and word search.

Atmosphere Games

AB
Sea Breezelocal wind from water to land during the day
Valley Breezelocal wind from valley up mountain during the day
Monsoonwet/rainy season....Summer months
Daytimewhen a sea breeze or valley breeze occurs
Droughtperiod of very little rain....winter months
Nighttimewhen a land breeze occurs
Summerseason of monsoons
Winterseason of droughts
Landheats up and cools down very fast
watertakes a long time to heat up or cool down
unequal heatingthe reason we have global and local winds
doldrumsweak wind belt at the equator
trade windsstrong winds that occur between 0° - 30° in each hemisphere
prevailing windssteady winds belt that is found from 40° to 60° in each hemisphere
polar windsweak winds found in each hemisphere between 60° - 90°
0° - 30°location of the trade winds in each hemisphere
40° - 60°location of the prevailing westerlies in each hemisphere
direct contacthow energy is transferred in conduction
electromagnetic waveshow energy is transferred through radiation
horse latitudesthe nickname for 30°
coriolis effectthe bending of winds in either hemisphere due to the rotation of the earth
greenhouse effectthe warming of the earth's surface and atmosphere due to heating from the sun's rays
carbon dioxide0.3% of our atmosphere's compotion
atmospherethe collection of gases that surround the earth
biosphereall the living organisms on the earth
hydrosphereall of the water included in the earth system
oxygencomposes 21% of the atmosphere
land breezelocal wind that moves from land to sea at night
thermospherethe outermost layer of the earth's atmosphere where temperature rises and there are very few particles
nitrogenmost abundant element in our atmosphere
windmoves from areas of high pressure to areas of low pressure
water vaporcomposes 0-4% of our atmostphere
global windmajor wind belts that occur on the earth due to unequal pressure
21%amount of oxygen in our atmosphere
0-4%amount of water vapor in our atmosphere
0.3%amount of carbon dioxide in our atmosphere
air pressurethe pulling of the atmosphere toward earth due to gravity
gravitythe cause of air pressure
tropospherethe lowest layer of the atmosphere
tropopausethe dividing line between the troposphere and the stratosphere
stratospherethe second layer of the atmosphere which contains the ozone layer
stratopuasedividing line between the stratosphere and mesosphere
mesospherelayer of the atmosphere where meteors burn up (third layer)
mesopausedividing line between the mesosphere and thermosphere
ionospheresublayer of the thermosphere where auroras occur
exosphereoutermost layer of the thermosphere with no definite ending point
ozone layerlocated at the top of the stratosphere and absorbs uv radiation
radiationtransfer of heat in the form of electromagnetic waves
convectiontransfer of energy in a fluid
conductiontransfer of energy through direct contact
equatorwhere the doldrums are located
in a fluidwhere convection occurs
60°-90°location of the polar winds in each hemisphere
jet streamfast moving current of air within the troposphere that impacts weather
currentsup down movement of air in the atmosphere
78%amount of the atmosphere composed of nitrogen
local windsmall winds that are caused by unequal heating of land and water

This activity was created by a Quia Web subscriber.
Learn more about Quia
Create your own activities