Weather Alert in Minnesota
Winter Weather Advisory issued March 12 at 3:21AM CDT until March 13 at 7:00AM CDT by NWS Duluth MN
AREAS AFFECTED: North Cass; South Itasca; Northern Aitkin
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 3 and 5 inches. Winds gusting as high as 50 mph. * WHERE...Northern Aitkin, North Cass, and South Itasca Counties. This includes the Tribal Lands of the Mille Lacs Band, Big Sandy Lake area. * WHEN...From 1 PM this afternoon to 7 AM CDT Friday. * IMPACTS...Travel could be very difficult. The hazardous conditions could impact the Thursday evening and Friday morning commutes. Gusty winds could bring down tree branches. * ADDITIONAL DETAILS...Strong winds paired with intense snowfall rates will lead to greatly reduced visibility.
INSTRUCTION: Slow down and use caution while traveling. Call 511 or visit www.511mn.org for Minnesota road information.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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