Weather Alert in Wisconsin
Special Weather Statement issued March 15 at 8:06AM CDT by NWS Green Bay WI
AREAS AFFECTED: Vilas; Oneida; Forest; Florence; Northern Marinette County; Lincoln; Langlade; Menominee; Northern Oconto County; Door; Marathon; Shawano; Wood; Portage; Waupaca; Waushara; Southern Marinette County; Southern Oconto County
DESCRIPTION: An intense band of heavy snow continued this morning from Marshfield and Wausau northward to Rhinelander and then eastward through Shawano, Marinette, Oconto and Florence. Snowfall rates of 2 to 4 inches per hour were reported with this band of heavy snow. Reports out of Wausau, Junction City and Marshfield indicated that 8 to 13 inches has fallen so far. Thunder snow will be possible with this band while some sleet or freezing rain is possible towards Wautoma. The intense band of snow should continue for the rest of the morning. Snowfall rates of 2 to 4 inches per hour should continue. Motorist should encounter difficult conditions with snow covered roads and visibilities around 1/4 mile or less. There will likely be break in the heavier snow later this afternoon before another round of heavier snow arrives this evening. Winter Storm Warnings and Blizzard Warnings are in effect today into Monday.
INSTRUCTION: N/A
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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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