Weather Alert in Maine
Winter Weather Advisory issued February 10 at 1:30AM EST until February 11 at 4:00PM EST by NWS Gray ME
AREAS AFFECTED: Northern Oxford; Northern Franklin; Southern Oxford; Southern Franklin; Southern Somerset; Interior York; Central Interior Cumberland; Androscoggin; Kennebec; Coastal York; Coastal Cumberland; Interior Cumberland Highlands; Northern Coos; Southern Coos; Northern Grafton; Northern Carroll; Southern Carroll; Strafford
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 3 and 6 inches. * WHERE...Portions of south central, southwest, and western Maine and central and northern New Hampshire. * WHEN...From 7 PM this evening to 4 PM EST Wednesday. * IMPACTS...A weak weather system will bring a period of light snowfall to the region. Although snowfall amounts will be light, travel will still be impacted due to snowfall accumulations on untreated roads. Periods of moderate and heavy snow will combine with low visibility to create dangerous driving conditions. The hazardous conditions could impact the Wednesday morning commute.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions can be obtained by going to newengland511.org
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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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