Weather Alert in New York
Winter Storm Warning issued February 19 at 1:15PM EST until February 21 at 1:00PM EST by NWS Albany NY
AREAS AFFECTED: Hamilton; Southeast Warren; Bennington; Western Windham; Eastern Windham
DESCRIPTION: * WHAT...Wintry mixed precipitation expected including snow, sleet, and freezing rain. Total snow accumulations range 6 and 9 inches with a glaze up to one tenth of an inch of flat ice from freezing rain. * WHERE...In New York, Southeast Warren and Hamilton Counties. In Vermont, Bennington, Eastern Windham, and Western Windham Counties. * WHEN...From 10 AM Friday to 1 PM EST Saturday. * IMPACTS...Roads, and especially bridges and overpasses, will likely become slick and hazardous. Travel could be difficult. The hazardous conditions could impact the Friday evening commute. * ADDITIONAL DETAILS...Snowfall rates may reach 0.5 to 1 inches at times, especially Friday evening.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency.
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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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