Weather Alert in North Dakota
Special Weather Statement issued April 2 at 5:15AM CDT by NWS Bismarck ND
AREAS AFFECTED: Divide; Burke; Renville; Bottineau; Rolette; Williams; Mountrail; Ward; McHenry; Pierce; McKenzie; Dunn; Mercer; Oliver; McLean; Sheridan; Golden Valley; Billings; Stark; Morton; Burleigh; Slope; Hettinger; Grant; Bowman; Adams; Sioux
DESCRIPTION: Areas of freezing drizzle and fog will impact much of western and central North Dakota early this morning. The freezing drizzle may deposit a thin layer of ice on untreated and elevated surfaces, such as sidewalks and bridges. Fog will be dense at times in southwest parts of the state, with visibility reduced to one quarter mile or less. Motorists should use caution on the morning commute and be prepared for rapidly changing conditions. Do not use cruise control and leave plenty of stopping distance ahead of you. Conditions are expected to improve by late morning.
INSTRUCTION: N/A
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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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