Weather Alert in Connecticut
Special Weather Statement issued September 6 at 4:19AM EDT by NWS Boston/Norton MA
AREAS AFFECTED: Hartford; Tolland; Windham; Western Franklin; Eastern Franklin; Northern Worcester; Western Hampshire; Western Hampden; Eastern Hampshire; Eastern Hampden; Southern Worcester; Northwest Middlesex County
DESCRIPTION: A cold front brings potential for scattered severe thunderstorms today to interior southern New England. Thunderstorms may begin to pop-up across eastern New York, along the border with Connecticut and Massachusetts early as 12-2pm. There after is prime time for storms to build develop,between 2-6pm, across the interior of southern New England. Expect thunderstorms to weaken as the line shifts to the I-95 corridor between 7-10pm. Thunderstorms will have the potential to produce straight-line damaging winds, hail, localized flash flooding in urban areas or locations of poor drainage, frequent lightning, and a lower risk of tornadoes. Whether you are heading to an outdoor event or hanging around the house, today is one of those days to remain weather aware, and have multiple ways of receiving weather alerts (cell phone notifications, NOAA Weather Radio, and broadcast meteorologists).
INSTRUCTION: N/A
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Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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