Weather Alert in Minnesota
Winter Weather Advisory issued March 5 at 11:24PM CST until March 7 at 6:00AM CST by NWS Aberdeen SD
AREAS AFFECTED: Traverse; Big Stone; Roberts; Codington; Grant; Hamlin; Deuel
DESCRIPTION: * WHAT...Mixed precipitation and patchy blowing snow expected. Total snow accumulations up to two inches and ice accumulations up to one tenth of an inch. Winds gusting as high as 35 mph. * WHERE...Portions of west central Minnesota and northeast South Dakota. * WHEN...From 10 AM Friday to 6 AM CST Saturday. * IMPACTS...Plan on slippery road conditions. Mainly drifting snow is expected, but in areas prone to blowing snow, the snow may be lofted and briefly reduce visibility. the combination of warm temperatures and drifting snow can cause snow to adhere to roads, creating icy patches. The hazardous conditions could impact the Friday evening commute.
INSTRUCTION: Slow down and use caution while traveling. In Minnesota, the latest road conditions can be obtained at 511mn.org, or by calling 5 1 1. In South Dakota, the latest road conditions can be obtained by calling 5 1 1.
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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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