Weather Alert in Kansas
High Wind Watch issued March 14 at 12:07AM CDT until March 15 at 9:00PM CDT by NWS Hastings NE
AREAS AFFECTED: Phillips; Smith; Jewell; Rooks; Osborne; Mitchell; Valley; Greeley; Nance; Sherman; Howard; Merrick; Polk; Dawson; Buffalo; Hall; Hamilton; York; Gosper; Phelps; Kearney; Adams; Clay; Fillmore; Furnas; Harlan; Franklin; Webster; Nuckolls; Thayer
DESCRIPTION: * WHAT...Sustained north-northwest winds at least 30 to 40 MPH, with frequent gusts at least 50 to 60 MPH. * WHERE...Portions of north central Kansas and central, east central, and south central Nebraska. * WHEN...From Sunday morning through Sunday evening. * IMPACTS...Damaging winds could damage trees and power lines. Travel could be difficult, especially for high profile vehicles. * ADDITIONAL DETAILS...Although any snow accumulation should remain well under 1 inch in most areas, areas of light snow on Sunday could combine with the strong winds to reduce visibility to under 1 mile at times, and also cause some slick spots on roads.
INSTRUCTION: Monitor the latest forecasts and warnings for updates. Fasten loose objects or shelter objects in a safe location prior to the onset of winds.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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