Weather Alert in Montana
Wind Advisory issued February 23 at 10:52PM MST until February 24 at 11:00AM 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 is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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