Weather Alert in Ohio
Cold Weather Advisory issued February 5 at 12:40PM EST until February 7 at 1:00PM EST by NWS Charleston WV
AREAS AFFECTED: Perry; Morgan; Athens; Washington; Jackson; Vinton; Meigs; Gallia; Mason; Jackson; Wood; Pleasants; Tyler; Roane; Wirt; Calhoun; Ritchie; Doddridge; Braxton; Gilmer; Lewis; Harrison; Taylor; Wyoming; Upshur; Barbour; Northwest Raleigh; Southeast Raleigh; Northwest Fayette; Southeast Fayette; Northwest Nicholas; Southeast Nicholas; Northwest Webster; Northwest Randolph
DESCRIPTION: * WHAT...Very cold wind chills as low as 14 below expected. * WHERE...Portions of southeast Ohio and central, northeast, northern, southeast, southern, and western West Virginia. * WHEN...From 1 AM to 1 PM EST Saturday. * IMPACTS...The cold wind chills as low as 15 below zero could result in hypothermia if precautions are not taken.
INSTRUCTION: Additional information can be found at https://www.weather.gov/rlx as well as on our X and Facebook pages.
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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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