Weather Alert in Michigan

Recent Locations: Sand Lake, NY   Elgin, OR   Drayton Plains, MI  

Special Weather Statement issued August 12 at 12:51AM EDT by NWS Grand Rapids MI

AREAS AFFECTED: Allegan; Van Buren

DESCRIPTION: At 1251 AM EDT, Doppler radar was tracking strong thunderstorms along a line extending from 14 miles west of South Haven to 5 miles northwest of Van Buren SP to 7 miles west of Shorewood-Tower Hill. Movement was northeast at 25 mph. HAZARD...Wind gusts up to 50 mph and penny size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor damage to outdoor objects is possible. Locations impacted include... Holland... Allegan... South Haven... Paw Paw... Wayland... Otsego... Plainwell... Hartford... Mattawan... Lawton... Bangor... Decatur... Fennville... Saugatuck... Martin... Van Buren SP... Lake Michigan Beach... Dorr... Pine Grove... Covert...

INSTRUCTION: If outdoors, consider seeking shelter inside a building. Torrential rainfall is also occurring with these storms and may lead to localized flooding. Do not drive your vehicle through flooded roadways. Frequent cloud to ground lightning is occurring with these storms. Lightning can strike 10 miles away from a thunderstorm. Seek a safe shelter inside a building or vehicle.

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Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

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

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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