Weather Alert in Maryland
Winter Storm Warning issued February 22 at 8:38AM EST until February 23 at 10:00AM EST by NWS Baltimore MD/Washington DC
AREAS AFFECTED: Carroll; Northern Baltimore; Cecil; Southern Baltimore; Anne Arundel; St. Marys; Calvert; Northwest Howard; Central and Southeast Howard; Northwest Harford; Southeast Harford
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations between 5 and 10 inches. Locally higher amounts up to 14 inches are possible in northeast Maryland. Northwest winds gusting between 35 and 45 mph overnight through Monday. Rain will change to snow between 4 PM and * WHERE...Portions of central, north central, northeast, northern, and southern Maryland. * WHEN...From 3 PM this afternoon to 10 AM EST Monday. Rain or a rain and snow mix will change to all snow between 3 PM and 6 PM this afternoon into this evening. Snow will continue tonight before tapering off Monday. * IMPACTS...Travel could be very difficult to impossible. The hazardous conditions will impact the Monday morning commute. * ADDITIONAL DETAILS...Visibility will be reduced to below one-half mile at times in falling and blowing snow overnight into Monday.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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