Weather Alert in Oklahoma
Flood Advisory issued June 15 at 2:32AM CDT until June 15 at 6:30AM CDT by NWS Norman OK
AREAS AFFECTED: Canadian, OK; Garfield, OK; Kingfisher, OK; Logan, OK
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Portions of central and northern Oklahoma, including the following counties, in central Oklahoma, Canadian, Kingfisher and Logan. In northern Oklahoma, Garfield. * WHEN...Until 630 AM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 231 AM CDT, Doppler radar indicated heavy rain due to thunderstorms. Minor flooding is ongoing or expected to begin shortly in the advisory area. Between 1 and 2 inches of rain have fallen in some locations. - Additional rainfall amounts up to 2 inches are expected over parts of the area. This additional rain will result in minor flooding. - Some locations that will experience flooding include... Northwestern Oklahoma City, Kingfisher, Piedmont, Hennessey, Cashion, Dover, Cedar Valley, Marshall, Cimarron City and Bison. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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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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