Weather Alert in New York
Flood Advisory issued April 2 at 4:58AM EDT until April 2 at 10:45PM EDT by NWS Buffalo NY
AREAS AFFECTED: Oswego, NY
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues along the Salmon River. * WHERE...A portion of central New York, including the following county, Oswego. * WHEN...Until 1045 PM EDT Thursday. * IMPACTS...Minor flooding in low-lying areas along the Salmon River will continue today. Fisherman should avoid the river with high flows creating dangerous conditions. * ADDITIONAL DETAILS... - At 454 AM EDT, gauge reports indicated high flows on the Salmon River resulting from recent heavy rainfall and snowmelt from the Tug Hill Plateau. Water releases will continue from the Salmon River Reservoir through at least today. - Some locations that will experience flooding include... Areas along the Salmon River from Altmar downstream through Pulaski to the mouth at Lake Ontario. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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