Forecast Details for Searsport, ME

Recent Locations: Searsport, ME  
Current Alerts for Searsport, ME: Coastal Flood Statement
Overnight: A slight chance of rain and sleet. Cloudy, with a low around 31. East wind around 5 mph. Chance of precipitation is 20%.
Friday: Rain and sleet, becoming all rain after 9am. High near 41. Northeast wind 5 to 15 mph. Chance of precipitation is 100%. Little or no sleet accumulation expected.
Friday Night: Rain. Low around 35. Calm wind becoming northwest around 5 mph. Chance of precipitation is 80%. New precipitation amounts between a tenth and quarter of an inch possible.
Saturday: A 30 percent chance of rain before 8am. Cloudy, with a high near 42. Northwest wind 10 to 15 mph, with gusts as high as 30 mph.
Saturday Night: Partly cloudy, with a low around 25. West wind 5 to 15 mph.
Sunday: Sunny, with a high near 47.
Sunday Night: Mostly cloudy, with a low around 28.
Monday: A chance of rain and snow showers. Partly sunny, with a high near 41. Chance of precipitation is 30%.
Monday Night: Partly cloudy, with a low around 18.
Tuesday: Sunny, with a high near 35.
Tuesday Night: Mostly clear, with a low around 17.
Wednesday: Sunny, with a high near 39.
Wednesday Night: Mostly clear, with a low around 22.
Thursday: Mostly sunny, with a high near 46.

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Weather Topic: What are Mammatus Clouds?

Home - Education - Cloud Types - Mammatus Clouds

mammatus clouds Next Topic: Shelf Clouds

A mammatus cloud is a cloud with a unique feature which resembles a web of pouches hanging along the base of the cloud.

In the United States, mammatus clouds tend to form in the warmer months, commonly in the Midwest and eastern regions.

While they usually form at the bottom of a cumulonimbis cloud, they can also form under altostratus, altocumulus, stratocumulus, and cirrus clouds. Mammatus clouds warn that severe weather is close.

Next Topic: Shelf Clouds

Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

wall clouds Next Topic: Condensation

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: Condensation