Weather Alert in Georgia

Recent Locations: Monterey Park, CA   Fairmont, MN   Tybee Island, GA  

Special Weather Statement issued March 24 at 2:01AM EDT by NWS Greenville-Spartanburg SC

AREAS AFFECTED: Rabun; Habersham; Stephens; Franklin; Hart; Elbert; Cherokee; York; Anderson; Abbeville; Laurens; Union; Chester; Greenwood; Oconee Mountains; Pickens Mountains; Greenville Mountains; Greater Oconee; Greater Pickens; Central Greenville; Southern Greenville; Northern Spartanburg; Southern Spartanburg

DESCRIPTION: Fuels remain quite dry across the region owing to breezy conditions and low relative humidity. Critical relative humidity is expected again today. Winds will be much less breezy on Tuesday afternoon than they were Monday; nonetheless, fire weather threat will be elevated by virtue of dry fuels and excessively low relative humidity. Outdoor fires will catch easily under these conditions. Please refer to your local burn permitting authorities on whether you can burn today. If you do burn, use extreme caution as fires can quickly get out of hand under these conditions.

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.

Next Topic: Condensation

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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