Weather Alert in Alaska

Recent Locations: Henagar, AL   Dolton, IL   Sand Point, AK  

Winter Weather Advisory issued February 24 at 2:07PM AKST until February 26 at 6:00AM AKST by NWS Juneau AK

AREAS AFFECTED: City and Borough of Juneau

DESCRIPTION: ...PERIODS OF SNOW THROUGH MID WEEK... .Light snow continuing in various inland areas this afternoon with around 2 to 4 inches already accumulated in Juneau and Petersburg. There should be a brief break in the snow tonight before more snow showers move in from the West Wednesday into Wednesday night. Snow accumulations will be highly variable Wednesday into Wednesday night with W to SW oriented slopes favored for higher snow totals. * WHAT...Snow. Additional snow accumulations of 4 to 10 inches. * WHERE...City and Borough of Juneau. * WHEN...Until 6 AM AKST Thursday. * IMPACTS...Travel could be very difficult and is discouraged. The hazardous conditions could impact the morning or evening commute. * ADDITIONAL DETAILS...Snow Tuesday afternoon and evening is expected to diminish Tuesday night, but will ramp back up Wednesday morning into Wednesday night. Snow accumulations will be highly variable with localized locations having a chance of seeing accumulations a few inches higher or lower then the above range.

INSTRUCTION: Slow down and use caution while traveling. People are urged to prepare their property before the onset of winter weather. For the latest road conditions, where available, call 5 1 1 or visit 511.alaska.gov.

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Weather Topic: What are Contrails?

Home - Education - Cloud Types - Contrails

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

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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