Weather Alert in New Jersey
Severe Thunderstorm Warning issued July 31 at 3:12PM EDT until July 31 at 4:00PM EDT by NWS Mount Holly NJ
AREAS AFFECTED: Burlington, NJ; Ocean, NJ
DESCRIPTION: SVRPHI The National Weather Service in Mount Holly NJ has issued a * Severe Thunderstorm Warning for... Northwestern Ocean County in southern New Jersey... East central Burlington County in southern New Jersey... * Until 400 PM EDT. * At 311 PM EDT, a severe thunderstorm was located near Cedar Glen Lakes, or 14 miles west of Toms River, moving northeast at 10 mph. HAZARD...60 mph wind gusts. SOURCE...Radar indicated. IMPACT...Damage to roofs, siding, trees, and power lines is possible. * Locations impacted include... Presidential Lakes Estates, Lakehurst, Cassville, Woodruff, Bamber Lake, Cedar Glen Lakes, Whiting, Pine Ridge At Crestwood, Browns Mills, Holiday City-Berkeley, Country Lake Estates, Crestwood Village, Holiday City, and Holiday Heights.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Torrential rainfall is occurring with this storm, and may lead to flash flooding. Do not drive your vehicle through flooded roadways.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
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
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