Weather Alert in Minnesota
Flood Warning issued July 28 at 8:43PM CDT by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Redwood, MN; Renville, MN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Minnesota... Minnesota River at Montevideo affecting Lac qui Parle, Yellow Medicine and Chippewa Counties. ...The Flood Warning continues for the following rivers in Minnesota... Minnesota River at Morton affecting Renville and Redwood Counties. * WHAT...Moderate flooding is forecast. * WHERE...Minnesota River at Morton. * WHEN...From Tuesday afternoon until further notice. * IMPACTS...At 24.0 feet, Fleischer Rd flooded in North Redwood; storm sewers closed off and bypass pumping begins. * ADDITIONAL DETAILS... - At 800 PM CDT Monday, the stage was 20.2 feet. - Forecast...The river is expected to rise above flood stage tomorrow afternoon and continue rising to a crest of 24.1 feet Friday morning. - Flood stage is 21.0 feet. - Flood History...This crest compares to a previous crest of 23.9 feet on 08/20/2017.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Caution is urged when walking near riverbanks.
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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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