Weather Alert in West Virginia
Special Weather Statement issued February 8 at 8:04PM EST by NWS Charleston WV
AREAS AFFECTED: Northwest Pocahontas; Southeast Pocahontas; Northwest Randolph; Southeast Randolph
DESCRIPTION: High pressure with clear, calm conditions atop the snowpack provide the perfect mid-winter setup for a frigid night and early Monday morning. Temperatures will bottom out in the single digits, single digits below zero in the normally colder low spots away from rivers, even isolated double digit lows below zero in the normally coldest sheltered mountain valleys, particularly for northern portions of Randolph and Pocahontas counties. Even with little or no wind, these low temperatures can lead to frostbite in as little as 30 minutes on exposed skin, as well as hypothermia. Bundle up if you must venture outside anytime tonight through early Monday morning, including the morning commute and bus run. If traveling, be prepared in case of a breakdown.
INSTRUCTION: N/A
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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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