Weather Alerts for Virginia
1. Blizzard Warning for: Accomack
2. Blizzard Warning for: Northampton
3. Winter Storm Warning for: Caroline; New Kent; James City; Western King William; Eastern King William; York
4. Winter Storm Warning for: Northern Fauquier
5. Winter Storm Warning for: Northern Virginia Blue Ridge; Central Virginia Blue Ridge
6. Winter Storm Warning for: Tazewell; Mercer; Summers
7. Winter Storm Warning for: Westmoreland; Richmond; Northumberland; Lancaster; Gloucester; Middlesex; Mathews; Western King and Queen; Eastern King and Queen; Western Essex; Eastern Essex
8. Winter Weather Advisory for: Bland; Giles; Bath; Monroe; Eastern Greenbrier
9. Winter Weather Advisory for: Dickenson; Buchanan
10. Winter Weather Advisory for: Eastern Hanover
11. Winter Weather Advisory for: Eastern Highland; Eastern Pendleton
12. Winter Weather Advisory for: Goochland; Nottoway; Amelia; Powhatan; Dinwiddie; Prince George; Charles City; Western Louisa; Eastern Louisa; Western Hanover; Western Chesterfield; Eastern Chesterfield (Including Col. Heights); Western Henrico (Including the City of Richmond); Eastern Henrico
13. Winter Weather Advisory for: Newport News; Hampton/Poquoson
14. Winter Weather Advisory for: Rappahannock; Culpeper; Stafford; Spotsylvania; King George; Southern Fauquier
15. Winter Weather Advisory for: Rockbridge; Amherst
16. Winter Weather Advisory for: Sussex; Surry; Southampton; Isle of Wight; Norfolk/Portsmouth; Suffolk; Chesapeake; Virginia Beach
17. Winter Weather Advisory for: Wise; Russell; Washington
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Current U.S. National Radar--Current
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North America Water Vapor (Moisture)
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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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