Weather Alert in Montana
Wind Advisory issued February 24 at 3:23AM MST until February 24 at 11:00AM MST by NWS Billings MT
AREAS AFFECTED: Livingston Area; Beartooth Foothills
DESCRIPTION: * WHAT...For the Wind Advisory, southwest winds gusting up to 60 mph. For the High Wind Watch, west winds gusting 65 to 75 mph possible. * WHERE...Beartooth Foothills and Livingston Area. * WHEN...For the Wind Advisory, until 11 AM MST this morning. For the High Wind Watch, from late tonight through Friday morning. * IMPACTS...Strong crosswinds will make travel difficult along Interstate 90 from Livingston to Big Timber and roads along the Beartooth Foothills. * ADDITIONAL DETAILS...Winds will decrease with the passage of a cold front early this morning. Periods of strong winds are expected to develop again late tonight and continue into Friday.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution and consider postponing travel until winds subside, or take an alternate route. Secure loose outdoor items.
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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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