Weather Alert in Connecticut
Special Weather Statement issued March 22 at 8:46PM EDT by NWS Boston/Norton MA
AREAS AFFECTED: Hartford; Tolland; Windham; Northern Worcester; Central Middlesex County; Western Hampshire; Western Hampden; Eastern Hampshire; Eastern Hampden; Southern Worcester; Western Norfolk; Southeast Middlesex; Suffolk; Eastern Norfolk; Northern Bristol; Western Plymouth; Eastern Plymouth; Northwest Providence; Southeast Providence; Western Kent; Eastern Kent; Bristol
DESCRIPTION: Ongoing areas of rain are expected to change to a slushy wintry mix of sleet and snow between 2 to 4 AM Monday, and then taper off between 9 to 11 AM Monday. Total snow and sleet accumulations of a coating to 2 inches are anticipated, primarily on grassy non-paved surfaces. It is possible that embedded heavier precipitation bands could lead to slushy accumulations on pavement, which would impact travelers during the Monday morning commute. This wintry precipitation should be mainly focused within about 20 miles either side of the Massachusetts Turnpike, but could extend as far south as the Hartford to Providence corridor. Motorists and commuters travelling during the pre-dawn hours into Monday morning should be aware of this changeover to wintry precipitation and the potential for slippery conditions. Travel with extra caution if snow and sleet is encountered Monday morning.
INSTRUCTION: N/A
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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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