Weather Alert in Minnesota
Flood Warning issued July 28 at 11:51AM CDT by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Chippewa, MN; Lac qui Parle, MN; Yellow Medicine, MN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Minnesota... Minnesota River at Montevideo affecting Yellow Medicine, Chippewa and Lac qui Parle Counties. .The river forecast remains on track at Montevideo. However, the timing and stage height forecast is subject to change depending on how much rainfall this area receives through tonight. * WHAT...Minor flooding is forecast. * WHERE...Minnesota River at Montevideo. * WHEN...From late tonight until further notice. * IMPACTS...At 17.0 feet, Storm sewers may need to be plugged to prevent water from backing up into streets. * ADDITIONAL DETAILS... - At 1100 AM CDT Monday, the stage was 13.5 feet. - Forecast...The river is expected to rise above flood stage late tonight and continue rising to 15.9 feet Monday, August 04. Additional rises are possible thereafter. - Flood stage is 14.0 feet. - Flood History...This crest compares to a previous crest of 15.9 feet on 07/11/1995.
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 Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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