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JH22-EARTH SYSTEMS VIII VOCAB-WEATHER II

ASSIGNED MONDAY (12/5)-LOG 15 MINUTES BY 10 PM THURSDAY

AB
CLIMATElong-term average of weather in an area
WEATHERday-to-day changes in atmospheric conditions, including temperature, air pressure, humidity, wind, cloud coverage, or precipitation
AIR MASSlarge body of air with the same temperature and humidity
FRONTwhere two different air masses meet normally causing precipitation
HUMIDITYamount of moisture in the air
JET STREAMfast moving stream of wind where cold, polar air meets warm air from the equator
ANEMOMETERtool that measures wind speed
BAROMETERtool that measures air pressure
WIND VANEtool that measures wind direction
AIR PRESSUREthe pressure caused by the weight of a column of air pushing down on an area
CONDENSATIONthe process by which molecules of water vapor in the air become liquid water
CORIOLIS EFFECTthe change that Earth's rotation causes in the motion of objects and that explains how winds curve
EVAPORATIONthe process by which water molecules in liquid water escape into the air as water vapor
PRECIPITATIONany form of water that falls from clouds and reaches Earth's surface
WATER CYCLEthe continual movement of water among Earth's atmosphere, oceans, and land surface through evaporation, condensation, and precipitation
DEW POINTthe temperature at which the water vapor in the air becomes saturated and condensation begins
COLD FRONTA front where cold air moves in under a warm air mass.
WARM FRONTForms when warm air slides up and over a cold air mass; it brings gentle rain or light snow followed by warmer weather.
HIGH PRESSUREA mass of sinking cool air that usually bring fair weather.
LOW PRESSUREA mass of rising warm air air that usually bring stormy weather.
WESTERLIESThe dominant winds that move across the USA
POLARdry, cold climate zone above 60 degree latitude
TEMPERATEseasonably variable climate zone between 40 and 60 degrees latitude, north or south of the equator
TROPICALwarm, moist climate zone near the equator
RELATIVE HUMIDITYa percentage of the maximum amount of water vapor the air can hold at its current temperature
TEMPERATUREMeasure of how hot or cold the air is. The closer to the equator you are, the warmer the temperature. Oceans and elevation also affect temperature.
WEATHERincludes temperature, precipitation, air pressure, wind and clouds. Powered by energy from the Sun and it is highly changeable. It changes from place to place and from hour to hour.
WINDmovement of air from on place to another. It is caused by differences in air pressure. Air flows from areas of high pressure to areas of low pressure. The greater the differences in air pressure the faster the wind.
CLOUDStiny visible water droplets of ice crystals high in the air
ISOTHERMline on the map joining up all the places with the same temperature.
CIRRUS CLOUDSthe most common of the high clouds. They are composed of ice and are thin, wispy clouds blown in high winds into long streamers
CIRROSTRATUS CLOUDSthin, sheetlike high clouds that often cover the entire sky. They are so thin that the sun and moon can be seen through them. These clouds usually come 12-24 hours before a rain or snow storm.
ALTOSTRATUS CLOUDSgray or blue-gray mid level clouds composed of ice crystals and water droplets. The clouds usually cover the entire sky. These clouds often form ahead of storms with continuous rain or snow.
ALTOCUMULUS CLOUDSmid level clouds that are made of water droplets and appear as gray puffy masses. They usually form in groups. If you see altocumulus clouds on a warm, sticky morning, be prepared to see thunderstorms late in the afternoon.
STRATUS CLOUDSuniform grayish clouds that often cover the entire sky. They resemble fog that doesn't reach the ground. Light mist or drizzle sometimes falls out of these clouds.
STRATOCUMULUS CLOUDSlow, puffy and gray. Most form in rows with blue sky visible in between them.
CUMULUS CLOUDSwhite, puffy clouds that look like pieces of floating cotton. These clouds are often called "fair-weather clouds". The base of each cloud is flat and the top of each cloud has rounded towers.
CUMULONIMBUS CLOUDSthunderstorm clouds. High winds can flatten the top of the cloud into an anvil-like shape. These clouds are associated with heavy rain, snow, hail, lightning and even tornadoes. The anvil usually points in the direction the storm is moving.
FOGa cloud on the ground. It is composed of billions of tiny water droplets floating in the air.
CONTRAILScondensation trails left behind jet aircrafts. These form when hot humid air from jet exhaust mixes with environmental air of low vapor pressure and low temperature. The mixing is a result of turbulence generated by the engine exhaust.


Physical Science/Biology Instructor
Winston Jr/Sr High School
Winston, MO

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