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Roland-Story Meteorology Chapter 5 --Matching

Chapter 5 -- Forms of condensation

AB
Bergeron processa theory that relates the formation of precipitation to supercooled clouds
Advection fogfog formed when warm mosit air is blown over a cool surface and chilled below the dew point
condensation nucleiare small particles about which cloud droplets form
cloudsis a visible mass of droplets or frozen crystals floating in the atmosphere above the surface of the Earth
cumulusis a type of cloud with noticeable vertical development and clearly defined edges
dewis water in the form of droplets that appears on thin, exposed objects in the morning or evening
fogis a cloud in contact with the ground
freezing nucleisolid particles that have a crystal form resembling that of ice
frostis the solid deposition of water vapor from saturated air
glazea layer of ice caused by freezing rain
hailis a form of precipitation which consists of balls or irregular lumps of ice
rainis a type of precipitation, a product of the condensation of atmospheric water vapor that is released on the Earth's surface
rimeis a coating of ice
sleetA mixture of snow and rain
snowis a type of precipitation in the form of crystalline water ice, consisting of a multitude of snowflakes that fall from clouds
steam fogfog having the appearance of steam
stratusis a cloud belonging to a class characterized by horizontal layering with a uniform base
super cooledwhen water droplets stay liquid even below freezing
upslope fogfog created when air moves up a slope and cools adiabatically
white frostis a solid deposition of ice which forms directly from water vapor contained in air
cirrusclouds are characterized by thin, wisplike strands, often accompanied by tufts, leading to their common name of 'mare's tail



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