Weather Alert in New York
Winter Weather Advisory issued February 10 at 12:39PM EST until February 11 at 7:00AM EST by NWS Burlington VT
AREAS AFFECTED: Northern St. Lawrence; Northern Franklin; Southeastern St. Lawrence; Southern Franklin; Western Clinton; Western Essex; Southwestern St. Lawrence
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 3 and 6 inches, with locally higher amounts in the northern Adirondacks. * WHERE...The St. Lawrence Valley and northern Adirondacks. * WHEN...Until 7 AM EST Wednesday. * IMPACTS...The heaviest snowfall rates are expected to occur this afternoon and during the evening commute. Slow travel conditions can be expected. Roads will likely become slick and hazardous. * ADDITIONAL DETAILS...Snowfall rates of 1 inch per hour are expected late this afternoon into early this evening.
INSTRUCTION: Slow down and use caution while traveling. For the latest on road conditions in New York, visit https://511ny.org.
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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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