Weather Alert in Virginia
Severe Thunderstorm Warning issued June 15 at 3:13PM EDT until June 15 at 4:00PM EDT by NWS Wakefield VA
AREAS AFFECTED: Prince George, VA; Surry, VA; Sussex, VA
DESCRIPTION: SVRAKQ The National Weather Service in Wakefield has issued a * Severe Thunderstorm Warning for... Central Prince George County in south central Virginia... North central Sussex County in southeastern Virginia... Northwestern Surry County in southeastern Virginia... * Until 400 PM EDT. * At 313 PM EDT, a severe thunderstorm was located over Disputanta, moving northeast at 25 mph. HAZARD...60 mph wind gusts. SOURCE...Radar indicated. IMPACT...Expect damage to trees and powerlines. * This severe thunderstorm will be near... Burrowsville and Cabin Point around 330 PM EDT. Claremont around 340 PM EDT. Other locations impacted by this severe thunderstorm include Taylors Corner, Spring Grove, Brandon, Gwaltney Corner, Oak Hill Corner, Savedge, Barham, and Prince George Golf.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Please report severe weather by calling 757-899-2415, posting to the NWS Wakefield Facebook page, or using X @NWSWAKEFIELDVA.
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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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