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Vocab. Ch.2.1

AB
weatherthe condition of the bottom layer of the earth's atmosphere in one place over a short time
atmospheremultilayered band of gases, water vapor, and dust above the earth
climatethe weather patterns that an area typically experiences over a long period of time
Greenhouse effectthe absorbtion of a small amount of solar radiation into the earth after the rest has been dispersed
rotationthe earth's spin on it's axis
axisthe invisible line through the center of the earth from pole to pole
revolutionone complete orbit around the sun
length of a year365.25 days
leap year--datethe year to account for the extra fourth of the time taken to revolve around the sun. Occurs every four years as the 366 day
Tropic of Cancerimaginary line at 23.5 degrees north
Tropic of Capricornimaginary line at 23.5 degrees south
summer/winter solsticethe halfway revolutions of the earth's path, when the sun's rays appear directly over the tropic of Cancer/Capricorn
spring/fall equinoxesthe halfway marks between the solstices where the sun's rays are directly over the equator. Lengths of day and night are equal
Climate zones: tropical, temperate, and polartropical: between 23.5 N & S: hot year round; temperate: between 23.5 and 66.5 N & S: wide range; polar: above/below 66.5 degrees: cold
precipitationall forms of water that fall from the atmosphere to the earth's surface
water cyclecycle of naturally recycling water through evaporation, condensation, and precipitation
convectional precipitationhot air rises from the earth's surface, cools, loses ability to hold water, precipitation forms. Common near equator and tropics
orographical precipitationwarm air passes over landforms, cools at top, precipitation forms. Common on coast
frontal precipitationtwo fronts of different temperatures meet, warmer rises and loses ability
frontsair masses
evaporationwater is heated enough to turn into gas
3 influences on climatelarge bodies of water, elevation, nearby landforms


Niccole

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