Weather Alert in Iowa
Special Weather Statement issued August 12 at 12:43AM CDT by NWS Quad Cities IA IL
AREAS AFFECTED: Iowa; Keokuk; Jefferson
DESCRIPTION: At 1243 AM CDT, Doppler radar was tracking strong thunderstorms along a line extending from 7 miles north of Ottumwa Industrial Airport to near Maharishi Vedic City. Movement was north at 45 mph. HAZARD...Winds in excess of 40 mph and minor flooding. SOURCE...Radar indicated. IMPACT...Gusty winds could cause minor tree limb damage and blow around unsecured objects. Slowing or redirecting of traffic due to ponding or flowing water. Closure of waterfront access due to flooding. Locations impacted include... Fairfield, Sigourney, North English, Hedrick, What Cheer, Richland, Batavia, Delta, Maharishi Vedic City, Keswick, South English, Packwood, Parnell, Millersburg, Harper, Martinsburg, Kinross, Hayesville, Abingdon, and Keota.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. Torrential rainfall is occurring and may lead to localized flooding. Do not drive your vehicle through flooded roadways.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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