onvection
The transfer of heat or moisture in a medium by the movement of a mass
or substance. When used to imply only upward vertical motion, it is then
the opposite of subsidence.
umulus
One of three basic cloud forms, this particular form is best known
for its vertical development. Cumulus are billowy clouds that often have
flat bases.
owndraft
A sudden descent of cool or cold air to the ground, usually with precipitation,
and associated with a thunderstorm or shower. The opposite of an updraft.
ry
Line
The boundary between the dry desert air mass of the Southwest and the
moist air mass from the Gulf of Mexico. It usually lies north-south across
the central and southern High Plains states during spring and summer. The
passage of a dry line results in a sharp decrease in humidity, clearing
skies, and a wind shift from southeasterly or south to southwesterly or
west. Its presence influences severe weather development in the Great Plains.
ust
Front
The leading edge of the cool, gusty surface winds produced by thunderstorm
downdrafts.
recipitation
All forms of water, liquid or solid that falls from clouds and reaches
the ground. This includes drizzle, freezing drizzle, freezing rain, hail,
ice crystals, ice pellets, rain, snow, snow pellets, and snow grains.
ubsidence
A sinking or downward motion of air, often seen in anticyclones. It
is most prevalent when there is colder, denser air aloft. It is often used
to imply the opposite of atmospheric convection.
upercell
A severe thunderstorm characterized by a rotating, long-lived, intense
updraft. Although not very common, they produce a relatively large amount
of severe weather, in particular, extremely large hail, damaging straight-line
winds, and practically all violent tornadoes.
pdraft
A small scale current of air with vertical motion. If there is enough
moisture, then it may condense, forming a cumulus cloud and possibly thunderstorms.
The opposite of a downdraft.
ind
shear
The rate of wind speed or direction change with distance. Vertical
wind shear is the rate of change of the wind with respect to altitude.
Horizontal wind shear is the rate of change on a horizontal plane.
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