Weather Alert in Michigan
Flood Watch issued April 2 at 12:50PM EDT until April 6 at 2:00PM EDT by NWS Grand Rapids MI
AREAS AFFECTED: Newaygo
DESCRIPTION: ...The National Weather Service in Grand Rapids MI has issued a Flood Watch for the following rivers in Michigan... Muskegon River at Newaygo affecting Newaygo County. Muskegon River at Bridgeton affecting Newaygo County. .1 To 2 inches of rain has fallen in recent days, with an additional 1 to 2 inches expected over the next few days. The Muskegon River has begun to rise, and flooding may develop by this weekend. * WHAT...Flooding is possible. * WHERE...Muskegon River at Bridgeton. * WHEN...From late Saturday night to early Monday afternoon. * IMPACTS...At 13.0 feet, Water overflows the banks into wooded areas. * ADDITIONAL DETAILS... - At 10:00 AM EDT Thursday the stage was 9.8 feet. - Forecast...Flood stage may be reached early Sunday morning. - Flood stage is 13.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Residents and those with interests near the river should monitor rising water levels and be prepared for possible flood warnings. Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. Additional information is available at www.weather.gov/grr.
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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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