Weather Alert in New York
Flood Watch issued March 11 at 2:11PM EDT until March 12 at 5:00PM EDT by NWS Buffalo NY
AREAS AFFECTED: Jefferson; Lewis
DESCRIPTION: * WHAT...Flooding caused by rain and snowmelt continues to be possible. * WHERE...A portion of central New York, including the following counties, Jefferson and Lewis. * WHEN...Through Thursday afternoon. * IMPACTS...Excessive runoff from snowmelt and rainfall may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Ice jams will also be possible in areas where significant ice remains. * ADDITIONAL DETAILS... - Between an inch and an inch and a half of rain is expected from last night through tonight. This combined with warm weather will result in snow melt, with a deep snow pack in place across the Black River basin. This will cause rises on the Black River, Moose River, Independence River, and Beaver River as well as other tributaries. There is a risk of flooding due to high flows or ice jams. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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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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