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Catalina eddy. The Catalina eddy wind pattern, also called the "coastal eddy " or "marine layer," is a localized weather phenomenon that occurs in the Southern California Bight, the mostly concave portion of the Southern California coast running from Point Conception to San Diego. The Catalina eddy leads to June Gloom, which is so much a part ...
A weak, shallow layer of clouds hovering over the coast of California, typical of the dissipation of the marine layer later in the day. The low-altitude stratus clouds that make up the June Gloom cloud layer form over the nearby ocean, and are transported over the coastal areas by the region's prevailing westerly winds. [1]
Marine weather forecasting is the process by which mariners and meteorological organizations attempt to forecast future weather conditions over the Earth 's oceans. Mariners have had rules of thumb regarding the navigation around tropical cyclones for many years, dividing a storm into halves and sailing through the normally weaker and more ...
Get the Seaside, CA local weather forecast by the hour and the next 10 days. ... (Reuters) -Monsoon rains hit the coast of India's southernmost state of Kerala on Thursday, two days sooner than ...
Coastal flooding and high surf warnings for the region are in effect through Saturday. View this post on Instagram A post shared by Pismo Beach Police Department (@pismo_beach_police_dept)
Get the Marina del Rey, CA local weather forecast by the hour and the next 10 days.
The Monterey Bay National Marine Sanctuary ( MBNMS) is a federally protected marine area offshore of California 's Big Sur and central coast in the United States. It is the largest US national marine sanctuary and has a shoreline length of 276 miles (444 km) stretching from just north of the Golden Gate Bridge at San Francisco to Cambria in San ...
Sea of fog riding the coastal marine layer through the Golden Gate Bridge at San Francisco, California Afternoon smog within a coastal marine layer in West Los Angeles. A marine layer is an air mass that develops over the surface of a large body of water, such as an ocean or large lake, in the presence of a temperature inversion.
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