Weather Alert in Alaska
Flood Advisory issued June 19 at 10:53AM AKDT until June 20 at 4:00PM AKDT by NWS Fairbanks AK
AREAS AFFECTED: Central Beaufort Sea Coast; Central Arctic Plains; Central Brooks Range
DESCRIPTION: * WHAT...Flooding caused by snowmelt continues. * WHERE...Sagavanirktok River along the Dalton Highway. * WHEN...Until 400 PM AKDT Friday. * IMPACTS...Flooding of rivers, creeks, streams and other low-lying and flood-prone locations is imminent or occurring. * ADDITIONAL DETAILS... - At 1049 AM AKDT, high water from rapid snowmelt over the past five days continues to cause erosion and minor flooding along the Sagavanirktok (Sag) River. - The USGS river gauge at MP 325 is now slowly receding. - High water will continue to move downstream over the coming days. Infrastructure near the river's mouth, including roads and bridges near the Deadhorse/Prudhoe Bay area is already being impacted. Water levels in this area are expected to gradually rise, particularly around high tide. - Motorists and local authorities are advised to monitor conditions closely and avoid flooded areas. - http://www.weather.gov/aprfc
INSTRUCTION: Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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