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 are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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