Weather Alert in Michigan
Flood Advisory issued April 27 at 8:39PM CDT until April 28 at 7:00PM CDT by NWS Marquette MI
AREAS AFFECTED: Marquette, MI
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Michigan... Michigamme River near Witch Lake affecting Dickinson and Marquette Counties. Michigamme River near Republic affecting Marquette County. * WHAT...Elevated river levels caused by rain and snowmelt continue. * WHERE...Michigamme River near Republic. * WHEN...Until tomorrow evening. * IMPACTS...At 7.7 feet, Water begins to impact the yards of homes near Bengtson bridge on County Road LI in South Republic * ADDITIONAL DETAILS... - At 10:17 AM EDT Sunday the stage was 8.6 feet. - Bankfull stage is 8.4 feet. - Forecast...The river is expected to slowly fall this week. - Action stage is 8.4 feet. - Flood stage is 9.0 feet. - www.weather.gov/safety/flood
INSTRUCTION: If you encounter a flooded roadway, turn around and find an alternative route. Additional information is available at www.weather.gov/marquette. The next statement will be issued Monday morning.Monday morning at 1100 AM CDT /noon EDT/.
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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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