Weather Alert in New York

Recent Locations: Clintondale, NY  

Special Weather Statement issued March 6 at 2:03AM EST by NWS Buffalo NY

AREAS AFFECTED: Wyoming; Chautauqua; Cattaraugus; Allegany; Southern Erie

DESCRIPTION: Regional observations indicate areas of fog across the Southern Tier early this morning, including portions of Interstate 86. Some of this fog is locally dense, with visibilities down to a quarter of a mile or less at times. Isolated spots in the deeper valleys may have temperatures at or slightly below freezing, this could allow for some slick spots on roads and bridges. If you will be traveling this morning, be sure to slow down and be prepared for rapid changes in visibility and the potential for black ice. The fog is expected to dissipate after sunrise.

INSTRUCTION: N/A

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Weather Topic: What is Evaporation?

Home - Education - Precipitation - Evaporation

Evaporation Next Topic: Fog

Evaporation is the process which returns water from the earth back to the atmosphere, and is another crucial process in the water cycle.

Evaporation is the transformation of liquid into gas, and it happens because molecules are excited by the application of energy and turn into vapor. In order for water to evaporate it has to be on the surface of a body of water.

Next Topic: Fog

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

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