Weather Alert in Nebraska
Special Weather Statement issued February 6 at 8:17PM CST by NWS Hastings NE
AREAS AFFECTED: Valley; Greeley; Nance; Sherman; Howard; Merrick; Polk; Buffalo; Hall; Hamilton
DESCRIPTION: Continued well-above normal temperatures (especially through Monday) will cause increasing ice melt along the Platte, North Loup, Middle Loup, South Loup and Loup Rivers in central and south central Nebraska. This could result in the possible formation of localized ice jams. Although not a certainty, should any ice jams happen to develop, water levels could fluctuate as much as 1 to 3 feet in a very short time, causing flooding with little, if any notice. If any ice jam flooding is observed over the next few days along the Platte or Loup River systems in central/south central Nebraska, please report it immediately to the National Weather Service in Hastings.
INSTRUCTION: N/A
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Weather Topic: What are Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
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
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