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Chapter 15 and 16 Re

Earth Science Book chapter 15 and 16 the atmosphere and Weather factors

QuestionAnswer
This is used to measure the condensed water vapor that falls to the Earth rain gauge
thin, high, feathery clouds made of ice crystals cirrus clouds
this is the difference in an aneroid barometer and mercury barometer mercury barometers have liquids
caused by differences in air pressure wind
layer of the atmosphere where we live troposphere
temperature at which water vapor condenses dew point
condensation on a solid surface dew
these make up the major wind belts global wind
instrument used to measure wind direction wind vane
layer of the atmosphere with the good ozone layer stratosphere
local wind in the daytime sea breeze
these are the three major types of clouds cumulus, stratus, cirrus
cool(cold) global winds polar westerlies
the Earth's atmosphere provides all of this needed so it is very important to living things gases
layer of the atmosphere with weather troposphere
cool air masses tend to be more or less dense less dense
as you rise farther in the atmosphere, this is what happens to the air pressure decreases
percent of oxygen in dry air 21%
local wind at night land breeze
layer of the atmmosphere where meteoroids burn up mesosphere
a colunm of mercury will do this as air pressure increases increase
local wind which moves from a body of water to land sea breeze
thin layer of gases that surround Earth atmosphere
since air has mass,the air in the atmosphere has this weight and density
layer of atmosphere where sattelites are located exosphere
instrument used to measure wind sped anemometer
Global areas that aare calm with no wind doldrums and horse latitudes
condition of Earth's atmosphere at a particular time and space weather
getting out of breat while climbing a mountain is caused by this less oxygen per a cubic meter(less density)
layer of atmophere with aurora borealis ionosphere
if a mass is less in a volume air, then this is also less density
this is a form of oxygen with three oxygen molucules ozone
these instruments are used to measure air pressure mercury and aneriod barometer
this type of wind blows over short distances local winds
layer of the atmosphere where weather balloons fly stratosphere
winds just above 30 degrees latitude prevailing westerlies
percent of nitrogen in dry air 78%
instrument used to measure relative humidity(wet and dry bulb) psychrometer
process by which gases hold heat in the atmosphere greenhouse effect
coldest layer of the atmosphere mesosphere
National Weather Service measures air pressure in these units millibars
the main layers of the atmosphere are classified according to their changes in this temperature
the acting on the roof of your house comes from air above and below the roof air pressure
local wind that moves from land to a body of water land breeze
layer of the atmosphere that gets waarmer as altitude increases stratosphere
ozone absorbs this type of electromagnetic radiation ultraviolet rdiation
fluffy, white clouds cumulus
type of slow electromagnet radiation felt as heat infrared radiation
large fluffy clouds that often produce thunderstorms cumulonimbus
frozen precipitation which is light and fluffy snow
energy source for winds on Earth sun
happens to dry air when heated rises
layered clouds which bring rain stratus
cloud low to the surface on cool mornings fog
frozen rain is also called this sleet
compact barometer with no liquid aneroid barometer
water is water in this state of matter gas
when the density of air increases, altitude... decreases
clouds formed by pollution photochemical smog
follows a disturbance in clouds thunderstorms
winds are caused by differences in this air pressure
forms when water vapor condenses on solid particles dew
any form of water which falls back to Earth's surface precipitation
winds above and below the equator trade winds
03 ozone
pressure does this as altitude increases decreases
winds that blow between the equator and poles global winds
as an air mass rises up a mountainside the temperature does this decreases
distance above sea level altitude
a clothes dryer is an example of what method of heat transfer convection
Created by: asif101
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