Weather Alert in Connecticut
Cold Weather Advisory issued February 8 at 8:47PM EST until February 9 at 10:00AM EST by NWS Albany NY
AREAS AFFECTED: Northern Litchfield; Southern Litchfield; Northern Berkshire; Southern Berkshire; Southern Herkimer; Southern Fulton; Montgomery; Northern Saratoga; Northern Washington; Schoharie; Western Schenectady; Eastern Schenectady; Southern Saratoga; Western Albany; Eastern Albany; Western Rensselaer; Eastern Rensselaer; Western Greene; Eastern Greene; Western Columbia; Eastern Columbia; Western Ulster; Eastern Ulster; Western Dutchess; Eastern Dutchess; Northern Fulton; Southeast Warren; Southern Washington; Bennington; Western Windham; Eastern Windham
DESCRIPTION: * WHAT...Very cold wind chills as low as 15 to 25 below with values as low as 25 to 29 below in the higher terrain areas of western New England, the Taconics, and the northern and eastern Catskills. * WHERE...Greater Capital District, Upper Hudson Valley, Mohawk Valley, the mid-Hudson Valley, northern and eastern Catskills, Helderbergs, Schoharie Valley, the Taconics and western New England. * WHEN...Until 10 AM EST Monday. * IMPACTS...The dangerously cold wind chills as low as 15 to 29 below zero could cause frostbite on exposed skin in as little as 10 to 30 minutes. Frostbite and hypothermia will occur if unprotected skin is exposed to these temperatures.
INSTRUCTION: Use caution while traveling outside. Wear appropriate clothing, a hat, and gloves. Keep pets indoors as much as possible.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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