Weather Alert in Arkansas
Special Weather Statement issued February 19 at 1:17AM CST by NWS Little Rock AR
AREAS AFFECTED: Fulton; Sharp; Stone; Izard; Independence; Cleburne; Conway; Faulkner; White; Perry; Garland; Saline; Pulaski; Pike; Clark; Hot Spring; Southeast Van Buren County; Northern Scott County; Northwest Yell County; Polk County Lower Elevations; Central and Eastern Montgomery County; Van Buren County Higher Elevations; Central and Southern Scott County; Yell Excluding Northwest; Northern Polk County Higher Elevations; Northern Montgomery County Higher Elevations; Southeast Polk County Higher Elevations; Southwest Montgomery County Higher Elevations
DESCRIPTION: Expect south to southwesterly winds around 10 to 20 mph by Thursday afternoon with some gusts in excess of 30 mph at times. Very dry air will be located over the area with minimum afternoon RH values between 15 to 30 percent. This will make it possible for wildfires to ignite and spread rapidly. Outdoor burning is not recommended. If a wildfire is observed, report it by dialing 911 or by contacting the Arkansas Forestry Division at (800) 468-8834.
INSTRUCTION: N/A
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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