Weather Alert in New York
Winter Weather Advisory issued March 22 at 2:30AM EDT until March 23 at 8:00AM EDT by NWS Burlington VT
AREAS AFFECTED: Northern Franklin; Southern Franklin; Western Clinton; Western Essex; Orleans; Essex; Lamoille; Caledonia; Washington; Orange; Eastern Chittenden; Eastern Addison; Eastern Rutland; Western Windsor; Eastern Windsor
DESCRIPTION: * WHAT...Snow and mixed precipitation. Total snow accumulation between 3 and 7 inches and ice accumulations around a light glaze. * WHERE...For the Adirondack region of northern New York and from the spine of the Green Mountains eastward in Vermont. * WHEN...Until 8 AM EDT Monday. * IMPACTS...Travel could be very difficult. The hazardous conditions could impact the Monday morning commute. * ADDITIONAL DETAILS...The heaviest snow will fall through 10 AM this morning. Snow may begin to mix with or change to rain at times this afternoon. Freezing drizzle will develop overnight tonight and continue into Monday morning.
INSTRUCTION: Slow down and use caution while traveling. For the latest on road conditions in Vermont, visit https://newengland511.org and for New York, visit https://511ny.org.
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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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