Weather Alert in Wisconsin
Winter Storm Watch issued March 13 at 2:06AM CDT until March 16 at 4:00PM CDT by NWS Green Bay WI
AREAS AFFECTED: Door
DESCRIPTION: * WHAT...For the Winter Storm Warning, heavy wet snow. Additional snow accumulations between 4 and 7 inches, highest across the northern Door Peninsula and Washington Island. Winds gusting as high as 45 mph. For the Winter Storm Watch, heavy snow possible. Total snow accumulations between 12 and 18 inches with localized totals in excess of 24 inches possible. Winds could gust as high as 45 mph. * WHERE...Door County. * WHEN...For the Winter Storm Warning, until 1 PM CDT this afternoon. For the Winter Storm Watch, from Saturday evening through Monday afternoon. * IMPACTS...For the Winter Storm Warning, plan on slippery road conditions. Patchy blowing and drifting snow could significantly reduce visibility. The hazardous conditions will impact the morning commute. Gusty winds could bring down tree branches. For the Winter Storm Watch Saturday night through Monday afternoon, the strong winds and weight of snow on tree limbs may down power lines and could cause sporadic power outages. Whiteout and near blizzard conditions are possible and may make travel treacherous and potentially life-threatening. Travel could be very difficult to impossible.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions can be obtained by calling 5 1 1. Monitor the latest forecasts for updates on the situation for Saturday night into Monday. People should consider delaying all travel. Motorists should use extreme caution if travel is absolutely necessary.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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