Weather Alert in Connecticut
Blizzard Warning issued February 22 at 6:55PM EST until February 23 at 7:00PM EST by NWS Albany NY
AREAS AFFECTED: Northern Litchfield; Southern Litchfield; Western Ulster; Eastern Ulster; Western Dutchess; Eastern Dutchess
DESCRIPTION: * WHAT...Blizzard conditions expected. Total snow accumulations between 12 and 18 inches. Winds gusting as high as 50 mph. * WHERE...Litchfield County in northwest Connecticut, Dutchess and Ulster Counties in eastern New York. * WHEN...Until 7 PM EST Monday. * IMPACTS...Travel will be difficult to impossible. The dangerous conditions will impact the Monday morning and evening commutes. Gusty winds could bring down tree limbs and power lines in addition to causing blowing and drifting snowfall. Visibility will drop as low as 1/4 mile. * ADDITIONAL DETAILS...A powerful nor'easter will impact the region tonight through Monday. The higher snowfall amounts will be favored across the higher elevations and far southern parts of the counties. Snowfall rates may reach 2 inches per hour at times late tonight into early Monday morning.
INSTRUCTION: Travel should be restricted to emergencies only. If you must travel, have a winter survival kit with you. If you get stranded, stay with your vehicle.
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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
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - 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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