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Published byRalph Holland Modified over 8 years ago
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Water in the Atmosphere
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Hydrological(Water) Cycle
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Hydrological Cycle vocabulary Evaporation: the process of converting a liquid to a gas Transpiration: process where plants absorb water through the roots and then give off water vapor through pores in their leaves Precipitation: any form of water that falls from a cloud to Earth’s surface(rain, snow, sleet, hail, glaze) Evapotranspiration: the rapid cycling of water vapor into the atmosphere by evaporation from Earth’s surface or by transpiration from plant leaves
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Hydrological Cycle vocabulary Sublimation: conversion of a solid directly to a gas without passing through the liquid state Infiltration: movement of surface water into rock or soil through cracks and pores Percolation: the movement and filtering of fluids through porous materials.filtering
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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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Deposition: process of water vapor turning directly into a solid Frost on a window pane
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Phase Changes : Turn to page 505 and copy figure 2 into your notes.
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Quick Check: Use the chart you drew to assist you. 1.Is energy lost or gained when a gas changes into a solid? 2.What is the above process called? 3. Name the process that occurs when ice cream absorbs 334 joules of energy? 4. Give an example of sublimation.
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Atmospheric Moisture Invisible in the form of water vapor gas (only what we can’t see) Where does it come from? Insolation(energy from the sun) -- heats water *changing it into a gaseous state Warm air can hold much more water than cold air
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Water vapor enters the atmosphere from the evaporation of water from oceans, lakes, marshes and glaciers
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Humidity: water vapor in the air Described as a. Specific humidity b.relative humidity
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Relative Humidity (The measure we encounter daily) Measure of the amount of water vapor present in air relative to the maximum amount that the air can contain at a given temperature (%) –e.g. if relative humidity is 50%, then it contains 1/2 the amount of water vapor it could hold at a given temperature Relative humidity decreases as temperature increases Temp. Increase, ability to hold water increases Then RH Decreases
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Relative Humidity and Temperature Figure 4.7, p. 125
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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 air is saturated with water vapor Dew, clouds, and fog forms If dew point is below freezing, frost will form
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Dew Point Temperature As air is cooled it eventually becomes saturated (100% relative humidity) the temperature of saturation is called the dew point temperature If cooling continues, condensation begins and dew forms
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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 precipitation: acid drops that fall to the ground - contain nitrate and sulfate particles that come from burning fuels, volcanoes and cars
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Rain gauge: instrument used to measure the amount of rainfall
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Cloud seeding: method to cause an increase in precipitation
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Condensation nuclei: suspended particles that provide the necessary surfaces for cloud forming condensation.
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