Weather Alert in New York
Special Weather Statement issued September 3 at 3:07PM EDT by NWS Burlington VT
AREAS AFFECTED: Northern Franklin; Eastern Clinton; Western Clinton; Eastern Essex; Grand Isle; Western Franklin; Orleans; Essex; Western Chittenden; Lamoille; Caledonia; Washington; Western Addison; Orange; Western Rutland; Eastern Franklin; Eastern Chittenden; Eastern Addison; Eastern Rutland; Western Windsor; Eastern Windsor
DESCRIPTION: Fine fuels remain very dry across the area, particularly across the Connecticut and Champlain Valleys, according to the Vermont Department of Forests, Parks and Recreation and the New York State Department of Environmental Conservation. Portions of central and northern Vermont and parts of northern New York also remain in moderate drought. Southerly winds will quickly increase to 10 to 15 MPH with gusts up to 25 MPH possible across Vermont. Localized gusts up to 35 MPH are possible particularly in the north to south oriented valleys of the Champlain Valley and portions of northern New York. This, combined with expected low relative humidity values between 25% to 35% will create near critical fire weather conditions Thursday. Winds will be strongest between noon and 8 PM, coinciding with the timing of the minimum relative humidity values. If any fires were to start the weather and fuel conditions could cause fires to quickly get out of control and be difficult to contain. Fire weather conditions areawide will quickly improve as confidence increases in wetting rainfall Thursday night. For more information about the current fire danger rating, any burn restrictions, and wildfire prevention and education, please visit your state forestry or environmental protection website.
INSTRUCTION: N/A
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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