Weather Alert in Michigan
Flood Advisory issued April 27 at 10:30AM EDT until April 28 at 8:00PM EDT by NWS Marquette MI
AREAS AFFECTED: Marquette, MI
DESCRIPTION: ...The Flood Advisory is extended for the following rivers in Michigan... Michigamme River near Republic affecting Marquette County. .Recent rainfall and snowmelt has lead to river rises above bankfull. * 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 fall to 6.3 feet Monday, May 05. - 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 this evening at 1000 PM EDT.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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