Weather Alert in Idaho
Severe Thunderstorm Warning issued August 29 at 1:54PM PDT until August 29 at 2:45PM PDT by NWS Spokane WA
AREAS AFFECTED: Bonner, ID; Boundary, ID; Pend Oreille, WA
DESCRIPTION: SVROTX The National Weather Service in Spokane has issued a * Severe Thunderstorm Warning for... Western Boundary County in the Panhandle of Idaho... Northwestern Bonner County in the Panhandle of Idaho... Eastern Pend Oreille County in northeastern Washington... * Until 245 PM PDT. * At 153 PM PDT, a severe thunderstorm was located 12 miles north of Nordman, moving south at 15 mph. HAZARD...60 mph wind gusts, quarter size hail, and very heavy rainfall rates. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * This severe thunderstorm will remain over mainly rural areas of western Boundary, northwestern Bonner and eastern Pend Oreille Counties.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Prepare immediately for large hail and deadly cloud to ground lightning. Seek shelter inside a well-built structure. Stay away from windows.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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