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Ch 15&16 Test Review

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Question
Answer
This is the difference in a aneroid barometer and a mercury barometer   rain gauge  
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thin, high feathery clouds made of ice crystals   cirrus clouds  
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This is the difference in a aneroid barometer and a mercury barometer   mercury has liquid in it  
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caused by differences in air pressure [density]   wind  
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layer of the atmosphere where we live   troposhere  
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temperature at which water vapor condenses   dew point  
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condensation on solid surfaces   dew  
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these make up the Earth's major wind belts   polar easterlies, trade winds and prevailing westerlies  
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instrument used to measure wind direction   wind vane  
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layer of the atomosphere with ozone   stratosphere  
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local wind in the daytime   sea breeze  
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these are the 3 major types of clouds   status and cirrus and cummulus  
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cool global winds   polar easterlies  
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3 O   Ozone  
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The earth's atmoshere provides all of this needed so it is very important to living things   gases  
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cool air masses tend to be more or less dense   more dense  
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As you rise farther in the atmosphere, this is what happens to the air pressure   decreases  
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percent of oxygen in dry air   21 percent  
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local wind at night   land breeze  
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layer where meteroids burn up   mesosphere  
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a column of mercury will do this as air pressure increases   rise  
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local wind which moves from a body of water to the land   sea breeze  
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this thin layer of gases surrounds the earth   atmosphere  
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since air has mass, the air in the atmosphere has this   density  
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layer containing satellites   exosphere  
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instrument used to measure wind speed   anemometer  
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global areas of calm   doldrums and horse latitudes  
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condition of earths atmosphere at a certain time and place   weather  
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getting out of breath when climbing a mountain is caused by this   less oxygen per cubic square  
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layer where the aurora borealis occurs   ionosphere  
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if mass is less in avolume then this is also less   density  
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form of oxygen with three oxygen atoms in each molecule   ozone  
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intruments that are used to measure air pressure   barometer  
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kinds of winds that blow over short distances   local winds  
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layer where weather ballons fly   stratosphere  
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winds just above the 30 degrees latitude   horse latitudes  
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percent of nitrogen in dry air   78 percent  
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instrument used to measure relative humidity   psycrometer  
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process by which gases hold heat in the atmosphere   green house effect  
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coldest layer   mesosphere  
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national weather service measures air pressure in these units   milli-bars  
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main layers are classified according to this   temperature  
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this acting on the roof of your house comes from air above and below the roof   pressure  
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local winds which moves from land to sea   land breeze  
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layer which gets warmer with altitude   stratosphere  
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ozone absorbs this kind of electromagnetic radiation   ultra violet radiation  
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fluffy white clouds   cummulus  
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type of electromagnetic radiation slower and felt as heat   infrared radiation  
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large flufffy clouf which often produce thunderstorms   cummulimbus  
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frozen precipitation which is light and fluffy   snow  
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energy soure for wind on the earth   sun  
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happens to dry air when heated   less dense rises  
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layered clouds which often bring rain   stratus  
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clouds low to the surface   fog  
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frozen rain   sleet  
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compact barometer with no liquid   aneroid  
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water vapor in which state of matter   gas  
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density of will increase the altitude does this   decrease  
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clouds formed from pollution   smog  
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follows a disterbence in the clouds   thunderstorms  
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winds are caused by   differences in air pressure  
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forms when water vapor condenses on solid particles   clouds  
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any form of water which fall to earths surface   precipitation  
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winds above and below the equator   trade winds  
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pressure does this as altitude increases   decreases  
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winds that blow between the equator and the poles   global winds  
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as an air mass rises up a mountainside the temperature does this   decrease  
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distance above sea level   altitude  
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a clothes dryer is an example of what methof of heat transfer   convection currents  
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