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9/22/14 1 Copyright © 2013 Pearson Education, Inc. The Atmosphere: An Introduction to Meteorology, 12 th Lutgens • Tarbuck Lectures by: Heather Gallacher, Cleveland State University Chapter 5: Forms of Condensation and Precipitation Copyright © 2013 Pearson Education, Inc. Copyright © 2013 Pearson Education, Inc. ! A cloud is a visible aggregate of small water droplets. " Condensation aloft: ! Adiabatic cooling causes clouds to form as water vapor condenses in the atmosphere. ! The air becomes saturated and there must be a surface. ! Condensation nuclei act as surfaces, on which the water vapor can condense. " Growth of cloud droplets: ! Hygroscopic (water-seeking) nuclei are most effective for condensation. ! Growth is rapid at first, then slows as water vapor is consumed. Copyright © 2013 Pearson Education, Inc. ! Clouds are classified on the basis of two criteria. " Form: ! Cirrus are high, white, and thin. ! Cumulus clouds are globular, usually exhibiting a flat base. ! Stratus clouds are best described as layers covering much of the sky. " Height: ! High clouds are above 6000 m. ! Middle clouds range between 2000–6000 m. ! Low clouds are at altitudes of less than 2000 m. ! Clouds of vertical development extend upward to span more than one height range.

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Page 1: Atmos 12e LO Ch05dallinlewis.weebly.com/uploads/1/3/2/4/13243743/ch5_ppt.pdf · Atmos_12e_LO_Ch05.ppt Author: Dallin Lewis Created Date: 9/23/2014 3:30:54 AM

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Copyright © 2013 Pearson Education, Inc.

The Atmosphere: An Introduction to Meteorology, 12th

Lutgens • Tarbuck

Lectures by:

Heather Gallacher, Cleveland State University

Chapter 5: Forms of Condensation and Precipitation

Copyright © 2013 Pearson Education, Inc.

Copyright © 2013 Pearson Education, Inc.

!  A cloud is a visible aggregate of small water droplets. "  Condensation aloft:

!  Adiabatic cooling causes clouds to form as water vapor condenses in the atmosphere.

!  The air becomes saturated and there must be a surface. !  Condensation nuclei act as surfaces, on which the water

vapor can condense. "  Growth of cloud droplets:

!  Hygroscopic (water-seeking) nuclei are most effective for condensation.

!  Growth is rapid at first, then slows as water vapor is consumed.

Copyright © 2013 Pearson Education, Inc.

!  Clouds are classified on the basis of two criteria. "  Form:

!  Cirrus are high, white, and thin. !  Cumulus clouds are globular, usually exhibiting a flat base. !  Stratus clouds are best described as layers covering much of

the sky. "  Height:

!  High clouds are above 6000 m. !  Middle clouds range between 2000–6000 m. !  Low clouds are at altitudes of less than 2000 m. !  Clouds of vertical development extend upward to span more

than one height range.

Page 2: Atmos 12e LO Ch05dallinlewis.weebly.com/uploads/1/3/2/4/13243743/ch5_ppt.pdf · Atmos_12e_LO_Ch05.ppt Author: Dallin Lewis Created Date: 9/23/2014 3:30:54 AM

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Copyright © 2013 Pearson Education, Inc.

Copyright © 2013 Pearson Education, Inc.

Copyright © 2013 Pearson Education, Inc.

!  High clouds: "  Cirrus "  Cirrostratus "  Cirrocumulus

!  Middle clouds: "  Altocumulus "  Altostratus

!  Low clouds: "  Stratus "  Stratocumulus "  Nimbostratus

!  Clouds of vertical development: "  Cumulonimbus "  Cumulus humilis "  Cumulus congestus

Page 3: Atmos 12e LO Ch05dallinlewis.weebly.com/uploads/1/3/2/4/13243743/ch5_ppt.pdf · Atmos_12e_LO_Ch05.ppt Author: Dallin Lewis Created Date: 9/23/2014 3:30:54 AM

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Copyright © 2013 Pearson Education, Inc.

!  Cloud varieties: "  Uncinus are hooked shaped clouds, often precursors to

bad weather. "  Fractus or fractured clouds are stratus or cumulus clouds

that appear broken. "  Mammatus clouds have udder-shaped protuberances on

their bottom surfaces and are associated with stormy weather.

"  Lenticular clouds are lens shaped and are common in rugged or mountainous topographies.

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!  Fog is defined as a cloud with its base at or very near the ground. "  Radiation "  Advection "  Upslope "  Evaporative

Copyright © 2013 Pearson Education, Inc.

!  Radiation fog results from radiation cooling of the ground and air. "  The high humidity can cause a small amount of cooling to

lower the temperature to the dew point. "  To be extensive, there should be a slight breeze. "  It is usually thickest in valleys.

!  Advection fog is a blanket of fog caused by warm, moist air blowing over a cold surface. "  Some turbulence is needed (10–30 kph winds).

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Copyright © 2013 Pearson Education, Inc.

!  Upslope fog is created when relatively humid air moves up a sloping landform or up the steep slopes of a mountain. "  The upward flow causes the air to expand and cool

adiabatically.

!  There are two types of evaporation fog. "  Frontal (precipitation) fog occurs when rain falls and

evaporates, saturating the cooler air below. "  Steam fog occurs when cool air moves over warm water.

!  Moisture evaporates and saturates the air above it. !  Steam fog is very common over lakes.

Copyright © 2013 Pearson Education, Inc.

Copyright © 2013 Pearson Education, Inc.

!  The Bergeron process (precipitation from cold clouds) depends on the coexistence of water vapor, liquid cloud droplets, and ice crystals.

Page 5: Atmos 12e LO Ch05dallinlewis.weebly.com/uploads/1/3/2/4/13243743/ch5_ppt.pdf · Atmos_12e_LO_Ch05.ppt Author: Dallin Lewis Created Date: 9/23/2014 3:30:54 AM

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!  The collision-coalescence process (precipitation from warm clouds) occurs as copious rainfall associated with clouds located below the freezing level (called warm clouds), especially in the tropics. "  Small droplets hit other droplets and become larger. "  They collide with more droplets and their falling velocity

increases.

Copyright © 2013 Pearson Education, Inc.

Copyright © 2013 Pearson Education, Inc.

Page 6: Atmos 12e LO Ch05dallinlewis.weebly.com/uploads/1/3/2/4/13243743/ch5_ppt.pdf · Atmos_12e_LO_Ch05.ppt Author: Dallin Lewis Created Date: 9/23/2014 3:30:54 AM

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Copyright © 2013 Pearson Education, Inc.

Copyright © 2013 Pearson Education, Inc.

!  Rain is restricted to droplets of water with a diameter at least 0.5mm.

!  Cloudbursts are unusually heavy rainfalls. !  Drizzle are fine, uniform droplets with a diameter

less than 0.5mm. !  Virga is rain that evaporates above ground. !  Mist contains the smallest droplets.

Copyright © 2013 Pearson Education, Inc.

!  Snow is precipitation in the form of ice crystals or aggregates of ice crystals.

!  Sleet is clear to translucent particles of ice, rain drops freeze while falling.

!  Freezing rain (glaze) are rain drops that become super-cooled, hit a surface, and freeze immediately.

Page 7: Atmos 12e LO Ch05dallinlewis.weebly.com/uploads/1/3/2/4/13243743/ch5_ppt.pdf · Atmos_12e_LO_Ch05.ppt Author: Dallin Lewis Created Date: 9/23/2014 3:30:54 AM

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Copyright © 2013 Pearson Education, Inc.

!  Hail is precipitation in the form of hard, rounded pellets of ice. "  It is produced in

cumulonimbus clouds. "  Hail stones begin as

small ice pellets and grow as they are propelled by updrafts and downdrafts through the cloud.

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!  Rime is a deposit of ice crystals, formed on surface objects by super-cooled fog or cloud droplets. "  It occurs when the surface temperature of an object is

below freezing.

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!  Standard instruments: "  A standard rain gauge catches rain water and conducts it

through a narrow opening into a cylindrical measuring tube. !  The gauge is 20 cm in diameter and can measure rainfall to the

nearest 0.025 cm. !  < 0.025 cm = trace

"  A tipping bucket has two compartments (or buckets). When one bucket fills, it tips and empties its water and the other bucket takes its place at the funnel.

"  A weighing gauge collects rain fall in a cylinder that rests on a spring balance. As the cylinder fills, the movement is transmitted to a pen that records the data.

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Copyright © 2013 Pearson Education, Inc.

!  When measuring snowfall, two measurements are normally taken. "  The depth is measured with a calibrated stick. "  To obtain the water equivalent, snow is melted and then

weighed or measured as rain.

!  Weather radar uses radio waves to measure precipitation. "  The radio waves penetrate small droplets, but are reflected

off larger ones. Echoes are sent back and displayed.

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!  Intentional weather modification, such as cloud seeding, is deliberate human intervention to influence processes that constitute the weather. "  Snow and rain making

!  Silver iodide crystals act as freezing nuceli. "  Fog and cloud dispersal

!  Cloud seeding with dry ice into super-cooled fog or stratus clouds helps to disperse them to improve visibility.

Copyright © 2013 Pearson Education, Inc.

!  Hail suppression has been shown to be ineffective. "  Anti-hail cannons produced a loud whistling noise and a

large smoke ring thought to suppress hail. "  Cloud seeding with silver iodide crystals was also

employed to disrupt the growth of hailstones. !  Several methods of frost prevention are being used.

"  Water sprinklers add heat from water and from the latent heat of fusion when the water freezes.

"  Air mixing uses wind machines to mix warm and cool air. "  Orchard heaters produce the most successful results, but

fuel cost can be significant.

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Copyright © 2013 Pearson Education, Inc.