Weather Alert in Michigan
Blizzard Warning issued March 14 at 2:04PM EDT until March 16 at 8:00PM EDT by NWS Marquette MI
AREAS AFFECTED: Gogebic
DESCRIPTION: * WHAT...Blizzard conditions expected. Total snow accumulations between 1 and 3 feet. Winds gusting as high as 40 mph. * WHERE...Gogebic County. * WHEN...From 1 AM Sunday to 7 PM CDT Monday. * IMPACTS...Travel will be treacherous and potentially life-threatening. Widespread blowing snow and heavy snowfall rates will significantly reduce visibility. Gusty winds could bring down tree branches and result in power outages. * ADDITIONAL DETAILS...Heavy snowfall rates of 1 to 2 inches per hour are expected much of the day Sunday. Strongest winds late Sunday afternoon into Monday.
INSTRUCTION: Travel should be restricted to emergencies only. If you must travel, have a winter survival kit with you. If you get stranded, stay with your vehicle.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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