Weather Alert in Alaska
Flood Watch issued August 25 at 8:10PM AKDT until August 26 at 4:00PM AKDT by NWS Fairbanks AK
AREAS AFFECTED: Southern Seward Peninsula Coast; Interior Seward Peninsula; Eastern Norton Sound and Nulato Hills
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...Including the following areas, Eastern Norton Sound and Nulato Hills, Interior Seward Peninsula and Southern Seward Peninsula Coast. This includes the cities of Nome, White Mountain, Golovin, Serpentine Hot Springs, Council, Haycock, Pilgrim Springs, Taylor, Unalakleet, Stebbins, St Michael, Elim, Koyuk, And Shaktoolik. * WHEN...Through Tuesday afternoon. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - Heavy rainfall is expected across the interior and southern Seward Peninsula as well as the eastern Norton Sound Monday afternoon through Tuesday. Rainfall amounts of 2 to 3 inches are forecast across the region, resulting in rapid rises along rivers, creeks, and streams. Smaller streams may see water rises to near or above flood stage overnight Monday night through Tuesday morning. - Http://www.weather.gov/aprfc
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop. Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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