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The Atmosphere: An Introduction to Meteorology, 12th
Lutgens • Tarbuck
Lectures by:
Heather Gallacher, Cleveland State University
Chapter 5: Forms of Condensation and Precipitation
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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.
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! 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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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
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! 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
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! 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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! 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.
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! The Bergeron process (precipitation from cold clouds) depends on the coexistence of water vapor, liquid cloud droplets, and ice crystals.
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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.
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! 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.
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! 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.
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! 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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! 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.
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! 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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