Weather Alert in Alaska
High Surf Advisory issued August 11 at 4:34AM AKDT until August 12 at 10:00PM AKDT by NWS Anchorage AK
AREAS AFFECTED: Kuskokwim Delta Coast and Nunivak Island
DESCRIPTION: * WHAT...Water levels 1 to 2 feet above the normal highest tide line. Wave heights between 4 to 8 feet along the coast. * WHERE...Along the Kuskokwim Delta Coast, including the communities of Kwigillingok, Kongiganak, and Kipnuk. * WHEN...From 10 AM AKDT Monday to 10 PM AKDT Tuesday. * IMPACTS...Localized coastal erosion may occur. * ADDITIONAL DETAILS...There will be 2 peaks of high water occurring around high tide. The first occurs this afternoon and the second on tomorrow afternoon. The strongest push of southerly winds into the coast, with gusts between 40 to 50 mph, will be this afternoon into tomorrow morning. However, southerly fetch and winds will linger through tomorrow evening causing wave heights to be slow to subside along the coast.
INSTRUCTION: A high surf advisory means that high surf will affect beaches in the advisory area, producing rip currents and localized beach erosion.
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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
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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