Weather Alert in North Dakota
Severe Thunderstorm Warning issued September 12 at 11:56PM CDT until September 13 at 12:45AM CDT by NWS Bismarck ND
AREAS AFFECTED: McKenzie, ND; Mountrail, ND
DESCRIPTION: SVRBIS The National Weather Service in Bismarck has issued a * Severe Thunderstorm Warning for... Northeastern McKenzie County in northwestern North Dakota... Southwestern Mountrail County in northwestern North Dakota... * Until 1245 AM CDT. * At 1156 PM CDT, a severe thunderstorm was located 11 miles northwest of Mandaree, or 22 miles east of Watford City, moving north at 25 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations impacted include... White Earth Bay Recreation Area and Charlson.
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
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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