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 is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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