Weather Alert in North Carolina
Special Weather Statement issued March 22 at 2:28PM EDT by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Alexander; Iredell; Davie; Catawba; Rowan; Cleveland; Lincoln; Gaston; Mecklenburg; Cabarrus; Union; Greater Caldwell; Greater Burke; Eastern McDowell; Greater Rutherford; Eastern Polk; 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: Dry brush and leaf litter have become very dry in recent days due to breezy conditions and low relative humidity. These conditions are forecast again tomorrow. Relative humidity will fall below 30 percent for much of the afternoon and wind gusts may reach 25 mph at times. Given the dry vegetation, outdoor fires will be able to spread quickly once started, increasing the danger of wildfires. Please refer to your local burn permitting authorities on whether you can burn today. If you do burn, use extreme caution since fires can quickly get out of hand under these conditions.
INSTRUCTION: N/A
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Weather Topic: What are Cirrostratus Clouds?
Home - Education - Cloud Types - Cirrostratus Clouds
Next Topic: Cirrus Clouds
Cirrostratus clouds are high, thin clouds that form above
20,000 feet and are made mostly of ice crystals. They sometimes look like giant
feathers, horse tails, or curls of hair in the sky.
These clouds are pushed by the jet stream and can move at high speeds reaching
100 mph.
What do they indicate?
They indicate that a precipitation is likely within 24 hours.
Next Topic: Cirrus Clouds
Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
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