Weather Alert in New York

Recent Locations: Philmont, NY  

Flood Warning issued March 8 at 10:40PM EDT until March 9 at 11:00AM EDT by NWS Burlington VT

AREAS AFFECTED: Clinton, NY; Essex, NY

DESCRIPTION: * WHAT...Flooding caused by rain and/or snowmelt and/or ice jam is expected. The River Flood Warning is being transitioned to a Flood Warning. * WHERE...A portion of northern New York, including the following counties, Clinton and Essex. * WHEN...Until 1100 AM EDT Monday. * IMPACTS...Flooding of rivers, creeks, streams, and other low-lying and flood-prone locations is imminent or occurring. * ADDITIONAL DETAILS... - At 1039 PM EDT, Emergency management reported an ice jam and heavy rain in the warned area due to Ice Jam. Flooding is ongoing or expected to begin shortly. - Ice has moved past Ausable Forks. Two jams have been reported downstream in Clintonville and Keeseville. These are currently not directly impacting anything, but photos depict ice near homes. Any release of water could cause flooding in the section of the Ausable River between Clintonville and Port Kent. Stay vigilant as ice jams can change very swiftly. - Some locations that will experience flooding include... Keeseville, AuSable, Chesterfield, Peru, Jay, Ausable Chasm, Clintonville and Ausable Point. - http://www.weather.gov/safety/flood

INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

Altocumulus Clouds Next Topic: Altostratus Clouds

Similar to cirrocumulus clouds, altocumulus clouds are characterized by cloud patches. They are distinguished by larger cloudlets than cirrocumulus clouds but are still smaller than stratocumulus clouds.

Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km) and may resemble, at times, the shape of a flying saucer. These uncommon formations, called altocumulus lenticularis, are created by uplift in the atmosphere and are most often seen in close proximity to mountains.

Next Topic: Altostratus Clouds

Weather Topic: What are Cirrocumulus Clouds?

Home - Education - Cloud Types - Cirrocumulus Clouds

Cirrocumulus Clouds Next Topic: Cirrostratus Clouds

Cirrocumulus clouds form at high altitudes (usually around 5 km) and have distinguishing characteristics displayed in a fine layer of small cloud patches. These small cloud patches are sometimes referred to as "cloudlets" in relation to the whole cloud formation.

Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the water droplets in the cloud freeze into ice crystals and the cloud becomes a cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud formations generally pass rapidly.

Next Topic: Cirrostratus Clouds

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