Weather Alert in Vermont
Air Quality Alert issued July 26 at 7:07AM EDT by NWS Burlington VT
AREAS AFFECTED: Grand Isle; Western Franklin; Orleans; Essex; Western Chittenden; Lamoille; Caledonia; Washington; Western Addison; Orange; Eastern Franklin; Eastern Chittenden; Eastern Addison
DESCRIPTION: The Vermont Agency of Natural Resources has issued an Air Quality Health Advisory for Code Red or Unhealthy for Everyone or greater category due to Fine Particulates for Caledonia, Eastern Addison, Eastern Chittenden, Eastern Franklin, Essex, Grand Isle, Lamoille, Orange, Orleans, Washington, Western Addison, Western Chittenden, and Western Franklin until 11 PM EDT this evening. The air quality index, or AQI, is expected to approach or exceed the Code Red or Unhealthy for Everyone or greater category due to Fine Particulates. Concentrations may drop slightly in the afternoon. Who needs to be concerned? All individuals may experience adverse respiratory symptoms. Sensitive groups may also experience aggravation of heart or lung disease. What should you do? The Vermont Department of Health recommends that all individuals should reduce prolonged or heavy exertion. It's okay to be active outside, but take more breaks and do less intense activities. Watch for symptoms such as coughing or shortness of breath. People with asthma should follow their asthma action plans and keep quick relief medicine handy. If you have heart disease: symptoms such as palpitations, shortness of breath, or unusual fatigue may indicate a serious problem. If you have any of these, contact your healthcare provider. For additional information, please visit the Vermont Agency of Natural Resources web site at https://dec.vermont.gov/air- quality/local-air-quality-forecasts.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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