Weather Alert in Kansas
Severe Thunderstorm Warning issued August 3 at 6:42PM CDT until August 3 at 7:45PM CDT by NWS Dodge City KS
AREAS AFFECTED: Finney, KS; Ford, KS; Gray, KS; Hodgeman, KS
DESCRIPTION: SVRDDC The National Weather Service in Dodge City has issued a * Severe Thunderstorm Warning for... Northern Ford County in southwestern Kansas... Northeastern Finney County in southwestern Kansas... Western Hodgeman County in southwestern Kansas... Northern Gray County in southwestern Kansas... * Until 745 PM CDT. * At 641 PM CDT, a severe thunderstorm was located 10 miles east of Kalvesta, moving south at 20 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. This will impact Dodge City Days festivities. * Locations impacted include... Dodge City.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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