Weather Alert in Minnesota
Winter Weather Advisory issued February 27 at 11:59AM CST until February 28 at 6:00PM CST by NWS La Crosse WI
AREAS AFFECTED: Wabasha; Winona; Buffalo; Trempealeau; Jackson; La Crosse; Monroe; Juneau; Adams
DESCRIPTION: ...BAND OF SNOW MOVES IN SATURDAY MORNING... .A narrow band of snow will move in from the west on Saturday morning and continue throughout much of the daytime hours. Snowfall rates of an inch an hour will be possible within the band resulting in quick accumulations on roadways. Snowfall amounts within the band will likely range between 2 to 4 inches with locally higher amounts of up to 6 inches possible. The exact location of the heaviest amounts still remains uncertain with a sharp cutoff in amounts possible over just a few miles. As a result, be sure to continue to monitor the forecast for updates as the location of snowfall amounts may still shift. * WHAT...Snow expected. Total snow accumulations between 1 and 4 inches. Locally higher amounts will be possible. * WHERE...Portions of southeast Minnesota and central and west central Wisconsin. * WHEN...From 6 AM to 6 PM CST Saturday. * IMPACTS...Plan on slippery road conditions.
INSTRUCTION: Slow down and use caution while traveling. In Minnesota, visit 511mn.org for road conditions. In Wisconsin, visit 511wi.gov 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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