Weather Alert in Virginia
Winter Weather Advisory issued March 2 at 6:39AM EST until March 3 at 7:00AM EST by NWS Baltimore MD/Washington DC
AREAS AFFECTED: Western Highland; Eastern Highland; Western Grant; Eastern Grant; Western Pendleton; Eastern Pendleton
DESCRIPTION: * WHAT...Mixed precipitation expected. Total snow accumulations of 1 to 3 inches and ice accumulations up to two tenths of an inch. The highest amounts will be along the ridges. * WHERE...Portions of western Virginia and eastern West Virginia. * WHEN...From 10 AM this morning to 7 AM EST Tuesday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions could impact the Monday evening and Tuesday morning commutes. * ADDITIONAL DETAILS...A period of snow is expected from late this morning into this afternoon. There may some breaks during the late afternoon and early evening before a wintry mix of snow, sleet, and then primarily freezing rain affects the area tonight. Precipitation will gradually change to plain rain and taper off Tuesday morning.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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