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 Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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