Weather Alert in Nevada
Special Weather Statement issued August 27 at 2:23PM PDT by NWS Reno NV
AREAS AFFECTED: Mineral and Southern Lyon Counties; Greater Lake Tahoe Area; Greater Reno-Carson City-Minden Area; Western Nevada Basin and Range including Pyramid Lake
DESCRIPTION: At 223 PM PDT, Doppler radar was tracking a cluster of strong thunderstorms over Dayton, or near Virginia City, moving east at 20 mph. HAZARD...Wind gusts up to 40 mph and pea size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor hail damage to vegetation is possible. Locations impacted include... Carson City, Virginia City, Dayton, Washoe City, Damonte Ranch, Pleasant Valley, Carson City Airport, Galena, New Washoe City, Indian Hills, Washoe Lake Campground, Us 395 At Douglas-Carson City Co Line, Lakeview, Rawe Peak, Gold Hill, Davis Creek Campground, Stewart, Junction U.S 50 And Six Mile Canyon-Ft Churchill Rd, Us 50 At Carson City-Lyon Co Line, and Junction U.S 50 And NV 341.
INSTRUCTION: If outdoors, consider seeking shelter inside a building.
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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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