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 Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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