Weather Alert in Kansas

Recent Locations: Coffeyville, KS  
Current Alerts for Coffeyville, KS: Flood Watch

Severe Thunderstorm Warning issued June 17 at 2:45AM CDT until June 17 at 3:30AM CDT by NWS Topeka KS

AREAS AFFECTED: Dickinson, KS

DESCRIPTION: SVRTOP The National Weather Service in Topeka has issued a * Severe Thunderstorm Warning for... Southwestern Dickinson County in central Kansas... * Until 330 AM CDT. * At 245 AM CDT, a severe thunderstorm was located 6 miles northeast of Gypsum, or 11 miles southwest of Abilene, moving east at 25 mph. HAZARD...70 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. 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... Hope and Carlton.

INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

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

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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