Weather Alert in Michigan
Winter Weather Advisory issued February 22 at 2:22PM EST until February 23 at 11:00AM EST by NWS Gaylord MI
AREAS AFFECTED: Presque Isle; Leelanau; Alpena; Benzie; Grand Traverse; Alcona; Manistee
DESCRIPTION: * WHAT...Snow. Additional snow accumulations up to 3 inches, locally as high as 4-5 inches. North winds gusting as high as 35 mph. * WHERE...Parts of northern Lower Michigan near the Lake Michigan and Lake Huron coasts. * WHEN...Until 11 AM EST Monday. * IMPACTS...Roads, and especially bridges and overpasses, could become snow-covered and hazardous, particularly with falling and blowing snow. Prepare for reduced visibilities and slick road conditions. The hazardous conditions could impact the Monday morning commute. * ADDITIONAL DETAILS...North to north-northwest winds will have the greatest impacts on roads oriented largely east-to-west, including the US-23 corridor between Cheboygan and Alpena.
INSTRUCTION: Slow down and use caution while traveling. Plan to leave extra travel time for the Monday morning commute.
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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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