Weather Alert in Vermont

Recent Locations: Sumter, SC   Adel, OR   Cuttingsville, VT  

Special Weather Statement issued September 4 at 4:31AM EDT by NWS Albany NY

AREAS AFFECTED: Bennington; Western Windham; Eastern Windham

DESCRIPTION: Fine fuels remain very dry across the area according to the Vermont Department of Forests, Parks and Recreation. Southerly winds today will increase to 10 to 15 mph with gusts up to 25 mph across southern Vermont. This, combined with expected low relative humidity values between 35 and 40 percent will create near critical fire weather conditions this afternoon. Winds will be strongest between noon and 8 PM, coinciding with the timing of the minimum relative humidity values. If any fires were to start, the weather and fuel conditions could cause fires to quickly get out of control and be difficult to contain. Fire weather conditions will quickly improve with a wetting rainfall expected this evening into tonight. For more information about the current fire danger rating, any burn restrictions, and wildfire prevention and education, please visit your state forestry or environmental protection website.

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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