Weather Alert in Montana

Recent Locations: Webster, PA   Homerville, GA   Dutton, MT  

Severe Thunderstorm Warning issued August 21 at 4:39AM MDT until August 21 at 5:30AM MDT by NWS Glasgow MT

AREAS AFFECTED: Dawson, MT; Richland, MT; Wibaux, MT

DESCRIPTION: SVRGGW The National Weather Service in Glasgow has issued a * Severe Thunderstorm Warning for... Northeastern Wibaux County in northeastern Montana... Eastern Dawson County in northeastern Montana... Southeastern Richland County in northeastern Montana... * Until 530 AM MDT. * At 437 AM MDT, severe thunderstorms were located along a line extending from 8 miles west of Lambert to 7 miles south of Glendive, moving east at 55 mph. HAZARD...60 mph wind gusts and nickel size hail. SOURCE...A 62 mph wind gust was recorded at Glendive Airport around 4:35 am. IMPACT...Expect damage to roofs, siding, and trees. * Locations impacted include... Sidney, Glendive, Wibaux, Savage, West Glendive, Lambert, Skaar, Intake, Enid, Wooley, Crane, Yates, Hodges, Forest Park, Stipek, Midway, and Burns.

INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.

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Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

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

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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