Weather Alert in Montana
High Wind Watch issued February 23 at 10:52PM MST until February 27 at 8:00AM MST by NWS Billings MT
AREAS AFFECTED: Livingston Area; Beartooth Foothills
DESCRIPTION: * WHAT...For the Wind Advisory, west winds 30 to 40 mph with gusts up to 65 mph occurring. For the High Wind Watch, west winds 35 to 45 mph with gusts up to 75 mph possible. * WHERE...Beartooth Foothills and Livingston Area. * WHEN...For the Wind Advisory, until 11 AM MST Tuesday. For the High Wind Watch, from late Tuesday night 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 begin to decrease with the passage of a cold front early Tuesday morning. Periods of strong winds are expected to develop again Wednesday and Thursday.
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 Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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