Weather Alert in Michigan
Special Weather Statement issued February 5 at 7:41PM EST by NWS Gaylord MI
AREAS AFFECTED: Emmet; Cheboygan; Presque Isle; Leelanau; Antrim; Otsego; Montmorency; Alpena; Benzie; Grand Traverse; Kalkaska; Crawford; Oscoda; Alcona; Manistee; Wexford; Missaukee; Roscommon; Ogemaw; Iosco; Gladwin; Arenac; Western Chippewa; Central Chippewa; Southeast Chippewa; Western Mackinac; Eastern Mackinac; Mackinac Island/Bois Blanc Island; Beaver Island and surrounding islands; Charlevoix
DESCRIPTION: Steadiest snowfall has shifted east of I-75 across northern lower and eastern upper Michigan. In the wake of the snowfall, areas of freezing drizzle have begun to mix in west of I-75 in northern lower Michigan and portions of eastern upper Michigan. This will continue eastward toward the Lake Huron shores of northern lower Michigan this evening, with freezing drizzle potential carrying into the overnight hours until the next round of snow builds into the region from the northwest between roughly 2:00am and 6:00am. As such, a glaze of ice is possible on all untreated surfaces through the evening into tonight. Be cognizant of weather conditions if you must travel this evening into tonight, as slippery surfaces may materialize on area roads, particularly on bridges and overpasses. Remember to increase your following distance in wintry weather, and to take it slow in ice and snow!
INSTRUCTION: N/A
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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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