Weather Alert in Maine

Current Alerts for Ocean Park, ME: High Surf Advisory Special Weather Statement

Special Weather Statement issued August 23 at 5:53AM EDT by NWS Gray ME

AREAS AFFECTED: Interior York; Central Interior Cumberland; Androscoggin; Kennebec; Interior Waldo; Coastal York; Coastal Cumberland; Sagadahoc; Lincoln; Knox; Coastal Waldo; Interior Cumberland Highlands; Strafford; Eastern Hillsborough; Interior Rockingham; Coastal Rockingham

DESCRIPTION: A dry air mass and breezy conditions will combine with very dry fuels such as grass, leaves, and twigs to create the potential for uncontrolled fire spread across coastal and interior Maine and southeast New Hampshire today. This afternoon, relative humidity values will decrease to levels between 30 to 40 percent. At the same time, southerly winds 10 to 15 mph with frequent gusts to 25 mph will continue to dry fuels and increase fire spread potential. Wind gusts are expected to slacken later this evening, but winds will remain breezy overnight. Extra caution should be taken to prevent wildfires. Always consult with fire officials before engaging in any open burning activities and comply with all applicable laws and regulations. Never leave an open fire unattended and always extinguish campfires completely before leaving.

INSTRUCTION: N/A

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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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