Weather Alert in Michigan
Flood Watch issued March 30 at 10:06AM EDT until April 3 at 2:00PM EDT by NWS Gaylord MI
AREAS AFFECTED: Wexford
DESCRIPTION: ...The National Weather Service in Gaylord MI has issued a Flood Watch for the following rivers in Michigan... Manistee River near Sherman affecting Wexford County. For the Manistee River...including Sherman...flooding is possible. * WHAT...Flooding is possible. * WHERE...Manistee River near Sherman. * WHEN...From Tuesday evening to early Friday afternoon. * IMPACTS...At 15.0 feet, Flooding begins around the Wilderness Canoe livery along left bank of river just downstream of M-37 bridge. * ADDITIONAL DETAILS... - At 9:30 AM EDT Monday the stage was 13.7 feet. - Forecast...Flood stage may be reached tomorrow evening. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you are in the watch area, remain alert to possible flooding. Additional information is available at www.weather.gov. The next statement will be issued by Tuesday morning at 1000 AM 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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