Weather Alert in New York

Recent Locations: New London, MN   Clintondale, NY  

Flood Warning issued March 9 at 12:06PM EDT until March 10 at 2:00PM EDT by NWS Buffalo NY

AREAS AFFECTED: Erie, NY; Niagara, NY

DESCRIPTION: ...The Flood Warning is extended for the following rivers in New York... Tonawanda Creek At Rapids affecting Niagara and Erie Counties. For the Tonawanda Creek...including Rapids...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Tonawanda Creek at Rapids. * WHEN...From Tuesday morning to early Tuesday afternoon. * IMPACTS...At 12.0 feet, Flood stage, lowland flooding of farm areas along Tonawanda Creek between Rapids and the Tonawanda Indian Reservation. Flooding may impact Fletcher, Burdick, Kelkenberg, and Tonawanda Creek Roads. * ADDITIONAL DETAILS... - At 11:00 AM EDT Monday the stage was 9.79 feet and rising. - Bankfull stage is 10.0 feet. - Forecast...The river is expected to rise to a crest of near 12.0 feet Tuesday morning. - Flood stage is 12.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: Caution is urged when walking near riverbanks. Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov. The next statement will be issued late tonight by 300 AM EDT.

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Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

Stratocumulus Clouds Next Topic: Stratus Clouds

Stratocumulus clouds are similar to altocumulus clouds in their fluffy appearance, but have a slightly darker shade due to their additional mass.

A good way to distinguish the two cloud types is to hold your hand out and measure the size of an individual cloud; if it is the size of your thumb it is generally an altocumulus cloud, if it is the size of your hand it is generally a stratocumulus cloud.

It is uncommon for stratocumulus clouds to produce precipitation, but if they do it is usually a light rain or snow.

Next Topic: Stratus Clouds

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

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