Weather Alert in Alaska
Wind Advisory issued August 22 at 11:03PM AKDT until August 24 at 1:00AM AKDT by NWS Fairbanks AK
AREAS AFFECTED: South Slopes Of The Eastern Brooks Range; South Slopes Of The Central Brooks Range; Dalton Highway Summits; White Mountains and High Terrain South of the Yukon River; Upper Chena River Valley; Chatanika River Valley
DESCRIPTION: * WHAT...Southwest winds 20 to 30 mph with gusts up to 45 mph expected. The strongest winds are expected above 2000 feet elevation. * WHERE...Chatanika River Valley, Dalton Highway Summits, South Slopes Of The Central Brooks Range, South Slopes Of The Eastern Brooks Range, Upper Chena River Valley, and White Mountains and High Terrain South of the Yukon River. * WHEN...From 4 AM Saturday to 1 AM AKDT Sunday. * IMPACTS...Gusty winds will blow around unsecured objects and may cause tree damage resulting in a few power outages. * ADDITIONAL DETAILS...These strong winds usher in a prolonged period of rainy weather so hunters and recreationists are encouraged to prepare for rising water levels on rivers and their tributaries.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution.
Want more detail? Get the Complete 7 Day and Night Detailed Forecast!
Current U.S. National Radar--Current
The Current National Weather Radar is shown below with a UTC Time (subtract 5 hours from UTC to get Eastern Time).
National Weather Forecast--Current
The Current National Weather Forecast and National Weather Map are shown below.
National Weather Forecast for Tomorrow
Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.
North America Water Vapor (Moisture)
This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.
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
Current conditions powered by WeatherAPI.com
