Weather Alert in Maine
Blizzard Warning issued February 22 at 3:46PM EST until February 23 at 10:00PM EST by NWS Gray ME
AREAS AFFECTED: Coastal York; Coastal Cumberland; Sagadahoc; Lincoln; Knox; Coastal Waldo
DESCRIPTION: * WHAT...Blizzard conditions expected. Total snow accumulations between 6 and 10 inches. Wind gusts in excess of 40 mph possible... especially along the immediate coast. * WHERE...Portions of south central and southwest Maine. * 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 through afternoon Monday. 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 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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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