Weather Alert in Michigan
Flood Warning issued March 31 at 9:07PM EDT until April 2 at 4:00AM EDT by NWS Gaylord MI
AREAS AFFECTED: Arenac, MI
DESCRIPTION: ...The National Weather Service in Gaylord MI has issued a Flood Warning for the following rivers in Michigan... Rifle River near Sterling affecting Arenac County. For the Rifle River...including Sterling...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Rifle River near Sterling. * WHEN...Until early Thursday morning. * IMPACTS...At 6.0 feet, High water begins to impact canoe livery at River View Campground. * ADDITIONAL DETAILS... - At 8:30 PM EDT Tuesday the stage was 5.8 feet. - Bankfull stage is 4.5 feet. - Forecast...The river will rise above flood stage late this evening to 6.5 feet tomorrow morning. It will then fall below flood stage late tomorrow evening to 4.7 feet early Friday morning. It will rise to 5.0 feet Friday evening. It will then fall again and remain below flood stage. - Flood stage is 6.0 feet. - Flood History...This crest compares to a previous crest of 6.5 feet on 05/18/2000. - http://www.weather.gov/safety/flood
INSTRUCTION: Caution is urged when walking near riverbanks. Additional information is available at www.weather.gov. Wednesday evening at 800 PM EDT.
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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
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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