Weather Alert in Iowa
Special Weather Statement issued May 9 at 4:46AM CDT by NWS Sioux Falls SD
AREAS AFFECTED: Lyon; Lincoln; Lyon; Murray; Cottonwood; Nobles; Jackson; Pipestone; Rock; Beadle; Kingsbury; Brookings; Jerauld; Sanborn; Miner; Lake; Moody; Brule; Aurora; Davison; Hanson; McCook; Minnehaha; Douglas; Hutchinson; Turner; Lincoln
DESCRIPTION: Warm and very dry conditions are expected this afternoon, with humidity levels as low as 15 to 25 percent. Coupled with breezy west to northwest winds gusting up to 20-25 mph, fire danger conditions may reach near critical levels. Fire danger will be greatest in localized areas where grasses are still receptive to fire starts and spread. Isolated to scattered light showers during the late afternoon and evening will also bring a potential for isolated gusts up to 40 to 50 mph. This could result in erratic fire behavior. Check with local officials before attempting any outdoor burning today.
INSTRUCTION: N/A
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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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