Weather Alert in Kansas
Heat Advisory issued June 21 at 2:37AM CDT until June 22 at 9:00PM CDT by NWS Hastings NE
AREAS AFFECTED: Phillips; Smith; Jewell; Rooks; Osborne; Mitchell; Dawson; Gosper; Phelps; Furnas; Harlan; Franklin; Webster
DESCRIPTION: * WHAT...Consecutive days of dangerously hot conditions with limited overnight relief. Heat index values peak between 101 to 108 degrees Saturday and between 98 to 103 degrees Sunday. * WHERE...Portions of north central Kansas and south central Nebraska. * WHEN...Until 9 PM CDT Sunday. * IMPACTS...Hot temperatures and high humidity may cause heat illnesses. * ADDITIONAL DETAILS...Overnight low temperatures will fall no lower than the mid to upper 70s, providing limited relief from the heat. Steady south winds may provide some relief for those outdoors, but dehydration and heat-related illnesses remain possible even in the windy conditions.
INSTRUCTION: Drink plenty of fluids, stay in an air-conditioned room, stay out of the sun, and check up on relatives and neighbors.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - 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
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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