Weather Alert in New York

Recent Locations: Philmont, NY  

Flood Watch issued March 12 at 1:41AM EDT until March 12 at 2:00PM EDT by NWS Albany NY

AREAS AFFECTED: Northern Herkimer; Hamilton; Southern Herkimer; Southern Fulton; Northern Saratoga; Northern Warren; Northern Washington; Northern Fulton; Southeast Warren

DESCRIPTION: * WHAT...Flooding caused by rain, snowmelt, and ice jams continues to be possible. * WHERE...The southwest Adirondacks, the western Mohawk Valley, and the Upper Hudson Valley. * WHEN...Through this afternoon. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Creeks and streams may rise out of their banks. Flooding may occur in poor drainage and urban areas. * ADDITIONAL DETAILS... - Mild temperatures over the past few days has allowed snow on the ground to ripen and melt. In addition, there have been periods of moderate to heavy rain. The combination of runoff from snow melt and rainfall will continue to result in rising rivers that will likely cause ice to break up and move, potentially resulting in ice jams and associated flooding. For more information on river forecasts, please visit water.noaa.gov. - 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 Cirrus Clouds?

Home - Education - Cloud Types - Cirrus Clouds

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

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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