Weather Alert in Iowa
Winter Weather Advisory issued March 6 at 7:24PM CST until March 7 at 9:00AM CST by NWS Des Moines IA
AREAS AFFECTED: Emmet
DESCRIPTION: ...WINTRY PRECIPITATION TONIGHT BEHIND STORMS IN FAR NORTHWEST IOWA... .Precipitation behind an incoming cold front will change to freezing rain or drizzle with potentially a brief burst of snow. Warmer road and surface temperatures will limit icing initially, with a light glaze of ice expected later this evening into tonight. Slick travel spots are expected. * WHAT...Mixed precipitation expected. Total ice accumulations up to one tenth of an inch. Total snow accumulations less than one half inch. * WHERE...Emmet County. * WHEN...Until 9 AM CST Saturday. * IMPACTS...Plan on slippery road conditions.
INSTRUCTION: Slow down and use caution while traveling. For the latest travel conditions, check the Iowa 511 app, www.511ia.org, or dial 511.
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North America Water Vapor (Moisture)
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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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