Weather Alert in Maine

Recent Locations: Lewiston, MN   Kenefic, OK   Temple, ME  
Current Alerts for Temple, ME: Winter Weather Advisory

Winter Weather Advisory issued April 4 at 1:46PM EDT until April 5 at 10:00AM EDT by NWS Gray ME

AREAS AFFECTED: Northern Oxford; Northern Franklin; Central Somerset; Northern Coos; Southern Coos

DESCRIPTION: * WHAT...Mixed precipitation expected. Total sleet accumulations around one tenth of an inch, and ice accumulations up to one tenth of an inch. Winds gusting as high as 40 mph. * WHERE...In Maine, Central Somerset, Northern Franklin, and Northern Oxford Counties. In New Hampshire, Northern Coos and Southern Coos Counties. * WHEN...From midnight tonight to 10 AM EDT Sunday. * IMPACTS...A period of mixed precipitation is expected with air temperatures remaining below freezing. Expect slippery road conditions and avoid travel if possible. Even light snowfall amounts can accumulate on roads and cause dangerous driving conditions due to snow covered roads. Gusty winds will blow around unsecured objects and break some tree limbs. The power outage threat is limited.

INSTRUCTION: Slow down and use caution while traveling. The latest road conditions can be obtained by going to newengland511.org

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Current U.S. National Radar--Current

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National Weather Forecast--Current

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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