Weather Alert in Oklahoma
High Wind Watch issued February 15 at 10:13AM CST until February 17 at 7:00PM CST by NWS Amarillo TX
AREAS AFFECTED: Cimarron; Texas; Beaver; Dallam; Sherman; Hansford; Ochiltree; Lipscomb; Hartley; Moore; Hutchinson; Roberts; Hemphill; Oldham; Potter; Carson; Gray; Deaf Smith; Randall; Armstrong; Palo Duro Canyon
DESCRIPTION: * WHAT...Southwest winds 35 to 40 mph with gusts up to 60 mph possible. * WHERE...The Oklahoma Panhandle and the Texas Panhandle, minus the far southeast Texas Panhandle. * WHEN...From Tuesday morning through Tuesday evening. * IMPACTS...Damaging winds could blow down trees and power lines. Widespread power outages are possible. Travel could be difficult, especially for high profile vehicles. * ADDITIONAL DETAILS...Strong winds may also produce blowing dust, which could cause a sudden drop in visibility.
INSTRUCTION: Monitor the latest forecasts and warnings for updates.
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Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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