Weather Alert in Minnesota
Winter Weather Advisory issued February 19 at 2:19AM CST until February 19 at 8:00AM CST by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Douglas; Stevens; Pope; Stearns; Swift; Kandiyohi; Meeker
DESCRIPTION: ...CONTINUED LIGHT SNOW TONING AND SNOW COVERED ROADS WILL LEAD TO A SLOW COMMUTE THURSDAY MORNING... .Snow will slowly diminish through the rest of tonight from Morris and Alexandria, east into the Twin Cities and far western Wisconsin. Additional snow accumulations will be up to 1 inch, though the light snow will result in continue snow covered roads in Thursday morning, which will result in a slow commute Thursday morning. * WHAT...Snow. Additional snow accumulations up to two inches. * WHERE...Kandiyohi, Meeker, Stearns, Douglas, Pope, Stevens, and Swift Counties. * WHEN...Until 8 AM CST this morning. * IMPACTS...Snow covered roads will lead to hazardous conditions impacting the Thursday morning commute.
INSTRUCTION: Slow down and use caution while traveling. Call 5 1 1 or visit 511mn.org for road conditions.
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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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