Weather Alert in Kansas
High Wind Warning issued February 17 at 2:32AM CST until February 17 at 6:00PM CST by NWS Dodge City KS
AREAS AFFECTED: Scott; Lane; Ness; Hamilton; Kearny; Finney; Hodgeman; Stanton; Grant; Haskell; Gray; Ford; Morton; Stevens; Seward; Meade; Clark
DESCRIPTION: * WHAT...Southwest to west winds 35 to 45 mph with gusts up to 70 mph expected. * WHERE...Portions of southwest and west central Kansas. * WHEN...From 11 AM CST /10 AM MST/ this morning to 6 PM CST /5 PM MST/ this evening. * IMPACTS...Strong to damaging winds will create widespread blowing dust reducing visibility. Travel will be very difficult, and dangerous for high profile vehicles. Minor structural damage and tree damage is possible. Sporadic power outages are possible.
INSTRUCTION: Remain in the lower levels of your home during the windstorm, and avoid windows. Watch for falling debris and tree limbs. Use caution if you must drive.
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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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