atmospheric moisture

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Atmospheric Moisture

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Atmospheric Moisture. Water in the atmosphere can be solid, liquid, or gas. Oceans supply most atmospheric moisture. Water enters the atmosphere through evapotranspiration and sublimation . Energy of Evapotranspiration. - PowerPoint PPT Presentation

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Page 1: Atmospheric Moisture

Atmospheric Moisture

Page 2: Atmospheric Moisture

• Water in the atmosphere can be solid, liquid, or gas.

• Oceans supply most atmospheric moisture.

• Water enters the atmosphere through evapotranspiration and sublimation.

Page 3: Atmospheric Moisture

Energy of Evapotranspiration• Large amounts of energy are required to change liquid

water into water vapor. • The most energetic molecules will leave the liquid during

evaporation.• Temperature of the remaining liquid is somewhat lower

than its surroundings.

Page 4: Atmospheric Moisture

HotWarmCold

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Page 7: Atmospheric Moisture

Process of Evaporation

Page 8: Atmospheric Moisture

What factors affect the rate at which water evaporates?

• Temperature

• Surface area of the water

• How saturated the air is

• Wind speed

Page 9: Atmospheric Moisture

What is Humidity?• Humidity: the water vapor in the atmosphere

• Absolute humidity: the amount(mass) of water vapor in each unit volume of air.

• Hotter air can hold MORE water vapor than colder air.

• Relative humidity: tells us “how full” the air is with water

Page 10: Atmospheric Moisture

Relative Humidity and Temperature

• At any given time and place, the air has a certain amount of water vapor (absolute humidity).

• If temperature changes, but amount of water vapor remains the same, the relative humidity will change.

• If temperature stays constant, but more water vapor is added to the air, absolute humidity AND relative humidity will increase.

Page 11: Atmospheric Moisture

Dew Point• Dew Point: the

temperature at which air is filled (saturated) with water vapor.

• If air temperature drops BELOW the dew point, water vapor in the air will condense to liquid water or sublimate into solid water.

Page 12: Atmospheric Moisture

How can we MEASURE relative humidity?

• Sling psychrometer• Hygrometer

• Both use 2 thermometers: wet bulb and dry bulb

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Page 15: Atmospheric Moisture

Cloud Formation• A cloud is a collection of

liquid water droplets and/or ice crystals suspended in the atmosphere and dense enough to be visible.

• Clouds form when the temperature cools below the dew point

Page 16: Atmospheric Moisture

Licancabur Volcano is located on the border between Chile and Bolivia.

Page 17: Atmospheric Moisture

• If a cloud is on, or just above, Earth’s surface, it is called FOG.

Page 18: Atmospheric Moisture

Cloud Formation• In addition to saturated air, clouds need a

condensation surface.

Page 19: Atmospheric Moisture

Precipitation• Precipitation: the falling

of liquid or solid water from clouds toward the surface of Earth.– Ice crystals or water

droplets must become big enough that they fall due to gravity.

• Rain Gauge: measures liquid precipitation

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Page 21: Atmospheric Moisture

Atmospheric Transparency• Atmospheric transparency: how

transparent the atmosphere is to insolation from the Sun.

• Haze: when the atmosphere has a very HIGH aerosol content (cloudless sky does not appear blue)– Smog: a haze that is highly

polluted; usually brownish

• Precipitation can clean the atmosphere

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