Weather Alert in Montana
Winter Storm Watch issued April 1 at 6:15AM MDT until April 4 at 6:00AM MDT by NWS Billings MT
AREAS AFFECTED: Southern Rosebud
DESCRIPTION: * WHAT...For the Winter Weather Advisory, mixed precipitation expected, including pockets of light freezing rain. Snow accumulations less than an inch. Ice accumulations of a light glaze. For the Winter Storm Watch, periods of heavy snow. Total snow accumulations between 4 and 8 inches possible. Winds could gust as high as 30 mph. * WHERE...Southern Rosebud. * WHEN...For the Winter Weather Advisory, until 9 AM MDT this morning. For the Winter Storm Watch, from late Thursday night through late Friday night. * IMPACTS...For the advisory, travel early this morning will be impacted by poor visibility and slick or slushy conditions on roads. This includes US-212 over Lame Deer Divide. For the Winter Storm Watch, difficult travel conditions due to snow, poor visibility and some blowing snow. Cool, wet and windy conditions will be hazardous for young livestock.
INSTRUCTION: Slow down and use caution while traveling. For the latest road conditions, call 5 1 1.
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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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