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 Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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