Weather Alert in Virginia
Special Weather Statement issued June 15 at 4:57PM EDT by NWS Wakefield VA
AREAS AFFECTED: Goochland; Powhatan; Western Hanover; Eastern Hanover; Western Chesterfield; Eastern Chesterfield (Including Col. Heights); Western Henrico (Including the City of Richmond); Eastern Henrico
DESCRIPTION: At 457 PM EDT, Doppler radar was tracking strong thunderstorms along a line extending from near Sabot to near Richmond. Movement was north at 20 mph. HAZARD...Wind gusts up to 40 mph and heavy rain. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Reduced visibility and minor flooding possible. Locations impacted include... Richmond, Ashland, Downtown Richmond, Bon Air, Virginia Union University, Virginia Commonwealth University, Tuckahoe, University Of Richmond, Mechanicsville, Bensley, Oilville, Manakin, East Highland Park, Glen Allen, Sabot, Laurel, Wyndham, Lakeside, Bellwood, and Crozier.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. Heavy rainfall is also occurring with these storms and may lead to localized flooding. Do not drive your vehicle through flooded roadways.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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