Weather Alert in New York

Recent Locations: Penn Yan, 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 Fractus Clouds?

Home - Education - Cloud Types - Fractus Clouds

Fractus Clouds Next Topic: Freezing Rain

A fractus cloud (scud) is a fragmented, tattered cloud which has likely been sheared off of another cloud. They are accessory clouds, meaning they develop from parent clouds, and are named in a way which describes the original cloud which contained them.

Fractus clouds which have originated from cumulus clouds are referred to as cumulus fractus, while fractus clouds which have originated from stratus clouds are referred to as stratus fractus. Under certain conditions a fractus cloud might merge with another cloud, or develop into a cumulus cloud, but usually a fractus cloud seen by itself will dissipate rapidly.

They are often observed on the leading and trailing edges of storm clouds, and are a display of wind activity.

Next Topic: Freezing Rain

Weather Topic: What is Graupel?

Home - Education - Precipitation - Graupel

Graupel Next Topic: Hail

Graupel is a form of precipitation that is created by atmospheric conditions which cause supercooled water droplets to contact snow crystals and freeze to their surface.

Sometimes known as soft hail or snow pellets, graupel is delicate and easily destroyed by touch. Whereas hail usually falls during severe weather, graupel doesn't require such conditions to form, and can form in mild precipitation similar to situations which produce snowfall.

Next Topic: Hail

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