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Water in the Atmosphere Chapter 18
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H 2 O exists in atmosphere in all three states of matter…
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Solid: snow hail ice
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Liquid: rain and cloud droplets
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Gas: invisible H2OH2O vapor
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H 2 O may change from one state to another:
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Melting: from solid ice to liquid H 2 O
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Freezing: liquid H 2 O to solid ice
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Evaporation: from liquid H 2 O to H 2 O vapor
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Condensation: from H 2 O vapor to liquid H 2 O
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Sublimation: change from solid to H 2 O vapor Example: Dry ice
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a measure of the energy in molecules the more energy the molecules have, the hotter it feels
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isotherm: lines on a map that connect places that have the same temperature
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thermometer: instrument that measures temperature alcohol and mercury thermometers used (mercury more accurate)
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water freezes at: 0ºC or 32 ºF water boils at: 100ºC or 212ºF
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Water vapor enters the atmosphere from the evaporation of water from oceans, lakes, marshes and glaciers
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Warmer the air, the more H 2 O vapor it can hold Humidity: water vapor in the air Relative humidity: the % of moisture the air can hold relative to the amount it can hold at a certain temperature
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Relative humidity=specific humidity X 100 capacity (saturated)
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Psychrometer: instruments used to measure relative humidity Works on principle that evaporation causes cooling 2 thermometers…wet- bulb and dry-bulb Readings show how dry the air is
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Dew point: the temperature at which water vapor condenses Dew, clouds, and fog forms If dew point is below freezing, frost will form
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Clouds: simply high fogs, mist, or haze Form when air above surface cools below dew point Shape depends on air movement that forms it:
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-horizontal air movement = layers -vertical air movement = piles
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Temperature above freezing – clouds drop water Temperature below freezing – clouds drop snow crystals
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Three main cloud types:
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CIRRUS: - thin, feathery, made of ice crystals - form at high altitudes - seen when weather is fair, but can mean rain or snow
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STRATUS Low sheets or layers; gray and smooth Block out the sun Associated with rain and drizzle
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CUMULUS Piled in thick, puffy masses Formed by vertically rising air currents Usually mean fair weather
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Other cloud types:
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Cirrostratus
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Stratocumulus
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Cirrocumulus
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Altocumulus
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Nimbostratus
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Cumulonimbus: large cloud that produce LIGHTNING, THUNDER, HEAVY SHOWERS = Thunderstorms
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Precipitation: Water that falls from the atmosphere to the earth Occurs when cloud droplets grow into drops heavy enough to fall to Earth
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FORMS OF PRECIPITATION Drizzle: fine drops, very close together, fall slowly ….less than 0.5mm diameter Rain drops: larger, farther apart, fall faster… 0.5mm to 5mm diameter Snow: falls in clumps of six-sided crystals Sleet: pellets of ice tha fall to the ground when raindrops fall through freezing air
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Hail: irregular balls or lumps made of layers of ice forms in cumulonimbus clouds-
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Acid rain: acid drops that fall to the ground - contain nitrate and sulfate particles that come from burning fuels, volcanoes and cars
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Cloud seeding: method to cause an increase in precipitation
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Rain gauge: instrument used to measure the amount of rainfall
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Condensation nuclei: suspended particles that provide the necessary surfaces for cloud forming condensation.
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