Weather Alert in Maine
Blizzard Warning issued February 22 at 12:51PM EST until February 23 at 10:00PM EST by NWS Gray ME
AREAS AFFECTED: Coastal York; Coastal Cumberland
DESCRIPTION: * WHAT...Blizzard conditions expected. Total snow accumulations between 6 and 9 inches. Wind gusts in excess of 40 mph possible... especially along the immediate coast. * WHERE...Coastal Cumberland and Coastal York Counties. * WHEN...From 7 AM to 10 PM EST Monday. * IMPACTS...Whiteout conditions are expected with visibilities below 1/4 mile due to falling and blowing snow. The greatest potential for blizzard conditions will exist late morning Monday through the afternoon hours. The hazardous conditions will arrive during the Monday morning commute and will continue through the evening commute. Strong winds will down tree limbs and blow around unsecured objects. A Few trees and power lines could be downed. The power outage threat is elevated.
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. The latest road conditions can be obtained by going to newengland511.org Persons should consider delaying all travel. Motorists should use extreme caution if travel is absolutely necessary.
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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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