Weather Alert in Georgia
Special Weather Statement issued August 12 at 1:05AM EDT by NWS Charleston SC
AREAS AFFECTED: Effingham; Tattnall; Evans; Inland Bryan; Coastal Bryan; Inland Chatham; Coastal Chatham; Long; Inland Liberty; Coastal Liberty; Inland McIntosh; Coastal McIntosh; Inland Jasper; Beaufort; Coastal Jasper
DESCRIPTION: Temperatures rising into the lower 90s combined with moderate to high levels of humidity will produce heat indices of 105 to 109 degrees for a brief period this afternoon. Isolated to scattered showers and thunderstorms may provide relief to some areas, especially away from the coast. If heat indices are expected to remain above 108 degrees or 2 hours or more, then a Heat Advisory will be issued.
INSTRUCTION: Take extra precautions if you work or spend time outside. When possible, reschedule strenuous activities to early morning or evening. Know the signs and symptoms of heat exhaustion and heat stroke. Wear light weight and loose fitting clothing when possible and drink plenty of water.
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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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