Weather Alert in New York

Recent Locations: Plainfield, IL   Chittenango, NY   New York City, NY  
Current Alerts for New York City, NY: Flood Advisory Flood Warning
High Wind Watch Wind Advisory

High Wind Watch issued March 14 at 1:29PM EDT until March 16 at 8:00PM EDT by NWS Buffalo NY

AREAS AFFECTED: Jefferson; Lewis

DESCRIPTION: * WHAT...South to Southeast winds 25 to 35 mph with gusts up to 60 mph possible through late Sunday night. Winds become southwest later Monday with a few gusts up to 50 mph. * WHERE...Jefferson and Lewis Counties. Strongest gusts Sunday night expected along the northwest and northern face of the Tug Hill. Strongest wind gusts Monday will be regionwide. * WHEN...From Sunday afternoon through Monday evening. Strongest gusts are expected Sunday night. * IMPACTS...Strong winds may blow down trees and power lines. Scattered power outages are possible. Travel may be difficult, especially for high profile vehicles.

INSTRUCTION: Monitor the latest forecasts and warnings for updates. Secure or shelter objects in a safe location prior to the onset of the strong winds.

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Current U.S. National Radar--Current

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National Weather Forecast--Current

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North America Water Vapor (Moisture)

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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