Weather Alert in Alaska
Flood Watch issued August 24 at 12:43PM AKDT until August 26 at 4:00PM AKDT by NWS Fairbanks AK
AREAS AFFECTED: South Slopes Of The Central Brooks Range; South Slopes of the Western Brooks Range; Upper Kobuk Valleys
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...Including the following areas, South Slopes Of The Central Brooks Range, South Slopes of the Western Brooks Range and Upper Kobuk Valleys. This includes the cities of Wiseman, Coldfoot, Chandalar Dot Camp, Iniakuk Lake, The Dalton Highway From Mp 165 To Mp 232, Walker Lake, Ambler, Shungnak, And Kobuk. * WHEN...From Monday afternoon 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 on Monday with light to moderate rainfall continuing through Tuesday. Rainfall amounts of 2 to 4 inches are forecast to be widespread across the watch area by Tuesday evening. Water levels are already high along the tributaries of the Koyukuk and Kobuk Rivers. The heavy rainfall is forecast to increase water levels to near or above flood stage by Monday night along smaller streams and rivers draining the south side of the Brooks Range. - 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 Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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