Weather Alert in Arkansas
Tornado Warning issued April 4 at 1:37AM CDT until April 4 at 2:15AM CDT by NWS Tulsa OK
AREAS AFFECTED: Crawford, AR
DESCRIPTION: TORTSA The National Weather Service in Tulsa has issued a * Tornado Warning for... West central Crawford County in northwestern Arkansas... * Until 215 AM CDT. * At 137 AM CDT, a severe squall line capable of producing tornadoes that may not be visible due to heavy rain was located 5 miles northeast of Roland, moving east at 35 mph. HAZARD...Tornado. SOURCE...Radar indicated rotation. IMPACT...Flying debris will be dangerous to those caught without shelter. Mobile homes will be damaged or destroyed. Damage to roofs, windows, and vehicles will occur. Tree damage is likely. * Locations in or near the path include... Figure Five... Dora... Furry... Cedarville... Rudy... Alma... Van Buren... This includes the following highways, Interstate 40 in Arkansas between mile markers 0 and 3, and between mile markers 12 and 13. Interstate 49 between mile markers 22 and 29.
INSTRUCTION: TAKE COVER NOW! Move to a basement or an interior room on the lowest floor of a sturdy building. Avoid windows. If you are outdoors, in a mobile home, or in a vehicle, move to the closest substantial shelter and protect yourself from flying debris.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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