Weather Alert in West Virginia

Recent Locations: Lost Creek, WV  

Flood Warning issued June 7 at 9:44AM EDT until June 7 at 1:30PM EDT by NWS Charleston WV

AREAS AFFECTED: Barbour, WV

DESCRIPTION: * WHAT...Flooding caused by prior excessive rainfall is expected. * WHERE...A portion of northern West Virginia, including the following county, Barbour. * WHEN...Until 130 PM EDT. * IMPACTS...Flooding of creeks, streams, roads, and other low-lying and flood-prone locations is imminent or occurring. * ADDITIONAL DETAILS... - At 941 AM EDT, emergency management reported lingering high water across the area from prior heavy rain this morning. Flooding is already occurring. - Some locations that will experience flooding include... Philippi and Nestorville. - http://www.weather.gov/safety/flood

INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Report flooding to the National Weather Service by calling toll free, 800 401 9535, when you can do so safely.

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Weather Topic: What is Condensation?

Home - Education - Precipitation - Condensation

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

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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