Weather Alert in Virginia
Special Weather Statement issued March 22 at 9:28AM EDT by NWS Wakefield VA
AREAS AFFECTED: Fluvanna; Prince Edward; Cumberland; Goochland; Caroline; Mecklenburg; Lunenburg; Nottoway; Amelia; Powhatan; Westmoreland; Richmond; Brunswick; Dinwiddie; Prince George; Charles City; New Kent; Western Louisa; Eastern Louisa; Western Hanover; Eastern Hanover; Western Chesterfield; Eastern Chesterfield (Including Col. Heights); Western Henrico (Including the City of Richmond); Eastern Henrico; Western King William; Eastern King William; Western King and Queen; Eastern King and Queen; Western Essex; Eastern Essex
DESCRIPTION: * TIMING: Until 7 PM this evening. * WINDS...Southwest 10 to 15 mph with gusts up to 20-25 mph. * RELATIVE HUMIDITY...As low as 25 to 30 percent. * TEMPERATURES...In the mid to upper 80s. * IMPACTS...Low relative humidities and breezy southwest winds could produce favorable conditions for wildfires to ignite and spread today. Residents are urged to exercise caution handling any potential ignition source, including machinery, cigarettes, and matches. Be sure to properly discard all smoking materials. Any dry grasses and tree litter that ignite will have the potential to spread quickly. Virginia residents are reminded that open burning is prohibited before 4 PM each day through April 30th.
INSTRUCTION: N/A
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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