Weather Alert in Connecticut
Winter Weather Advisory issued March 3 at 6:23PM EST until March 4 at 5:00AM EST by NWS Albany NY
AREAS AFFECTED: Northern Litchfield; Southern Litchfield; Northern Berkshire; Southern Berkshire; Northern Saratoga; Eastern Rensselaer; Eastern Columbia; Eastern Dutchess; Southeast Warren; Southern Washington; Bennington; Western Windham; Eastern Windham
DESCRIPTION: * WHAT...Mixed precipitation. Additional snow accumulations up to one inch and ice accumulations around one tenth of an inch. * WHERE...Northwestern Connecticut, western Massachusetts, Taconics and the Lake George Saratoga region of eastern New York, and southern Vermont. * WHEN...Until 5 AM EST Wednesday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will continue to impact the Tuesday evening commute. * ADDITIONAL DETAILS...Snow and wintry mix will continue this evening but will start to taper during the overnight hours. All precipitation should be done by the late night hours.
INSTRUCTION: Slow down and use caution while traveling.
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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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