Weather Alert in Vermont

Recent Locations: Avondale, AZ   Spalding, NE   Killington, VT  

Special Weather Statement issued September 3 at 3:17PM 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 will quickly 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 Thursday. 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 areawide will quickly improve as confidence increases in wetting rainfall Thursday night. 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 Cirrus Clouds?

Home - Education - Cloud Types - Cirrus Clouds

Cirrus Clouds Next Topic: Condensation

Cirrus clouds are high-level clouds that occur above 20,000 feet and are composed mainly of ice crystals. They are thin and wispy in appearance.

What do they indicate?
They are often the first sign of an approaching storm.

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Weather Topic: What are Contrails?

Home - Education - Cloud Types - Contrails

Contrails Next Topic: Cumulonimbus Clouds

A contrail is an artificial cloud, created by the passing of an aircraft.

Contrails form because water vapor in the exhaust of aircraft engines is suspended in the air under certain temperatures and humidity conditions. These contrails are called exhaust contrails.

Another type of contrail can form due to a temporary reduction in air pressure moving over the plane's surface, causing condensation. These are called aerodynamic contrails.

When you can see your breath on a cold day, it is also because of condensation. The reason contrails last longer than the condensation from your breath is because the water in contrails freezes into ice particles.

Next Topic: Cumulonimbus Clouds

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