Weather Alert in Kansas
Severe Thunderstorm Warning issued August 3 at 6:13PM CDT until August 3 at 7:00PM CDT by NWS Dodge City KS
AREAS AFFECTED: Finney, KS; Hodgeman, KS; Lane, KS; Ness, KS; Scott, KS
DESCRIPTION: SVRDDC The National Weather Service in Dodge City has issued a * Severe Thunderstorm Warning for... Northern Finney County in southwestern Kansas... Southeastern Scott County in west central Kansas... Southwestern Ness County in west central Kansas... Northwestern Hodgeman County in southwestern Kansas... Lane County in west central Kansas... * Until 700 PM CDT. * At 613 PM CDT, severe thunderstorms were located along a line extending from near Beeler to near Scott City, moving south at 40 mph. HAZARD...Golf ball size hail and 70 mph wind gusts. SOURCE...Radar indicated. IMPACT...People and animals outdoors will be injured. Expect hail damage to roofs, siding, windows, and vehicles. Expect considerable tree damage. Wind damage is also likely to mobile homes, roofs, and outbuildings. * Severe thunderstorms will be near... Shallow Water around 620 PM CDT. Friend around 625 PM CDT. Other locations in the path of these severe thunderstorms include Kalvesta.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Large hail, damaging wind, and continuous cloud to ground lightning are occurring with these storms. Move indoors immediately. Lightning is one of nature's leading killers. Remember, if you can hear thunder, you are close enough to be struck by lightning. Torrential rainfall is occurring with these storms, and may lead to flash flooding. Do not drive your vehicle through flooded roadways.
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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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