Weather Alert in Alaska
Winter Storm Warning issued February 23 at 3:34PM AKST until February 25 at 6:00AM AKST by NWS Fairbanks AK
AREAS AFFECTED: Upper Chena River Valley; Tanana Flats; Eielson AFB and Salcha; Goldstream Valley and Nenana Hills; Chatanika River Valley; Two Rivers; Fairbanks Metro Area; Nenana; Central Interior
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations between 12 and 18 inches. Winds could gust up to 30 mph. * WHERE...Central Interior, Nenana, Fairbanks North Star Borough * WHEN...Until 6 AM AKST Wednesday. * IMPACTS...Travel could be very difficult. * ADDITIONAL DETAILS...Multiple days of moderate snowfall expected, lasting through Tuesday night. The heaviest snow is expected Monday through Tuesday morning with lighter snowfall continuing through Tuesday night. Westerly winds strengthen through the Tanana Valley Tuesday which may lead to periods of blowing snow. Increased snow on frozen rivers and streams could lead to areas of overflow. Use caution while traveling on and along frozen waterways.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. Visit 511.alaska.gov or call 5 1 1 for the latest road conditions.
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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