Weather Alert in Oklahoma
Severe Thunderstorm Warning issued September 1 at 6:36PM CDT until September 1 at 7:15PM CDT by NWS Norman OK
AREAS AFFECTED: Custer, OK; Dewey, OK
DESCRIPTION: SVROUN The National Weather Service in Norman has issued a * Severe Thunderstorm Warning for... Northwestern Custer County in western Oklahoma... Dewey County in northwestern Oklahoma... * Until 715 PM CDT. * At 635 PM CDT, severe thunderstorms were located along a line extending from near Leedey to 3 miles southwest of Seiling, moving southeast at 30 mph. HAZARD...70 mph wind gusts and quarter size hail. SOURCE...The Camargo Mesonet measured a 74 mph wind gust. IMPACT...Hail damage to vehicles is expected. Expect considerable tree damage. Wind damage is also likely to mobile homes, roofs, and outbuildings. * Locations impacted include... Taloga, Seiling, Hammon, Leedey, Butler, Putnam, Moorewood, and Foss Reservoir.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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