Weather Alert in Minnesota
Winter Weather Advisory issued March 12 at 2:31PM CDT until March 13 at 4:00AM CDT by NWS Aberdeen SD
AREAS AFFECTED: Traverse; Big Stone
DESCRIPTION: * WHAT...For the Winter Weather Advisory, snow and patchy blowing snow expected. Total snow accumulations up to one inch. Winds gusting as high as 60 mph. For the Winter Storm Watch, heavy snow and widespread blowing snow possible. Total snow accumulations between 5 and 10 inches possible. Winds could gust as high as 40 mph. * WHERE...Big Stone and Traverse Counties. * WHEN...For the Winter Weather Advisory, from 10 PM this evening to 4 AM CDT Friday. For the Winter Storm Watch, from Saturday afternoon through Sunday evening. * IMPACTS...For both events, travel could be very difficult. Falling and blowing snow, frequently reducing visibility below a half mile, may make travel dangerous, especially in open country. Strong winds could cause tree damage.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions can be obtained at 511mn.org, or by calling 5 1 1. Monitor the latest forecasts for updates on this situation.
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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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