Weather Alert in Connecticut
Special Weather Statement issued March 7 at 12:17AM EST by NWS Albany NY
AREAS AFFECTED: Northern Litchfield; Southern Litchfield; Northern Berkshire; Southern Berkshire; Bennington; Western Windham; Eastern Windham
DESCRIPTION: Some patchy freezing drizzle may impact portions of western New England this morning, especially over the higher terrain. Since some temperatures in this area remain near or below freezing, especially in the higher elevations, a light glaze of ice could result in slippery travel conditions this morning on untreated surfaces. Motorists and pedestrians should remain aware of the possibility for icy surfaces this morning. Elevated roads such as bridges and overpasses, and highway on and off ramps will be particularly vulnerable to icing, as well as parking lots and other untreated walkways.
INSTRUCTION: N/A
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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