Weather Alert in Georgia
Special Weather Statement issued March 24 at 1:44AM 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 Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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