Weather Alert in Alaska
Hydrologic Outlook issued August 29 at 12:50PM AKDT by NWS Anchorage AK
AREAS AFFECTED: Northern Bristol Bay Coast
DESCRIPTION: ESFAFC Prolonged moderate to heavy rain from Togiak to Dillingham is expected Saturday afternoon through Monday morning. Lighter rain showers will begin as early as Saturday morning and will continue into Monday evening. Expect water levels along small streams and rivers to rise, especially in steeper terrain. Expected Rainfall: Saturday Morning through Monday afternoon * Togiak/Twin Hills: 3.5 inches. * Dillingham: 2.2 inches. * Manokotak: 2.7 inches. * Clarks Point: 2.1 inches. Hydrologic Concerns: * Higher than normal river and stream levels have already been noted. Higher than normal water levels may continue into Tuesday. * Many lower locations along rivers such as gravel bars are likely to become inundated with water. * Heavy rain may result in localized ponding in low-lying areas and locations with poor drainage. Next Steps: * Residents along area streams as well as river users should anticipate higher than normal water levels and are advised to monitor weather and river forecasts. * Reports on river conditions may be sent to the River Forecast Center by calling 1-800-847-1739.
INSTRUCTION: N/A
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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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