Weather Alert in Connecticut
Extreme Cold Watch issued February 5 at 12:51AM EST until February 8 at 1:00PM EST by NWS Albany NY
AREAS AFFECTED: Northern Litchfield; Southern Litchfield; Northern Berkshire; Southern Berkshire; Northern Saratoga; Northern Warren; Northern Washington; Eastern Schenectady; Southern Saratoga; Eastern Albany; Western Rensselaer; Eastern Rensselaer; Eastern Greene; Western Columbia; Eastern Columbia; Eastern Ulster; Western Dutchess; Eastern Dutchess; Southeast Warren; Southern Washington; Bennington; Western Windham; Eastern Windham
DESCRIPTION: * WHAT...Dangerously cold wind chills between 20 and 35 degrees below below possible. * WHERE...The Hudson Valley and Taconics in eastern New York and all of western New England. * WHEN...From Saturday evening through Sunday afternoon. * IMPACTS...The dangerously cold wind chills as low as 35 below zero could cause frostbite on exposed skin in as little as 10 minutes.
INSTRUCTION: Dress in layers including a hat, face mask, and gloves if you must go outside. To prevent water pipes from freezing; wrap or drain or allow them to drip slowly.
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - 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
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