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 Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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