Weather Alert in Delaware
Special Weather Statement issued February 28 at 4:17AM EST by NWS Mount Holly NJ
AREAS AFFECTED: New Castle; Kent; Inland Sussex; Delaware Beaches; Morris; Hunterdon; Somerset; Delaware; Philadelphia; Western Chester; Eastern Chester; Western Montgomery; Eastern Montgomery; Upper Bucks; Lower Bucks
DESCRIPTION: Areas of patchy fog have continued to expand into portions of Delaware, northern New Jersey, and southeast Pennsylvania early this morning. Temperatures are also below freezing, which may result in areas of freezing fog. In addition, any snowmelt from Friday could result in the formation of black ice. Use caution if traveling this morning as patchy fog can result in unexpected reduced visibilities and black ice can make conditions very slippery. Slow down, use your low beam lights, and leave extra room between you and other vehicles.
INSTRUCTION: N/A
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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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