Weather Alert in Maryland
Winter Weather Advisory issued February 24 at 10:36AM EST until February 25 at 10:00AM EST by NWS Baltimore MD/Washington DC
AREAS AFFECTED: Western Garrett; Eastern Garrett; Western Highland; Western Grant; Western Pendleton
DESCRIPTION: * WHAT...Snow is expected. Total snow accumulations of 3 to 5 inches; locally higher at elevations above 2500 feet. A light glaze of ice is also possible along the eastern facing ridges Wednesday morning into midday as temps warm to around freezing. Wind gusts between 35 to 45 mph; locally higher above 3500 feet. * WHERE...In Maryland, Eastern Garrett and Western Garrett Counties. In Virginia, Western Highland County. In West Virginia, Western Grant and Western Pendleton Counties. * WHEN...From 10 PM this evening to 10 AM EST Wednesday. * IMPACTS...Plan on slippery road conditions, especially along I-68/US-40 west of Frostburg, MD, WV-48 west of Moorefield, WV, US-33/WV-28 west of Franklin, WV, and US-25O west of Monterey, VA. The hazardous conditions could impact the Wednesday morning commute. Gusty winds could bring down tree branches and power-lines due to the heavier weight of the snow.
INSTRUCTION: Slow down and use caution while traveling. 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 is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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