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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.
Nassau received its first bulletin from the U.S. Weather Bureau on the morning of September 25, shortly before the onset of gale-force winds by noon and hurricane-force winds that evening. [22] Sustained winds at Nassau reached an estimated 120–140 mph (195–225 km/h), [ 22 ] punctuated by a maximum gust of 164 mph (264 km/h).
[57] [58] As of September 15, about 2,100 people remained in 20 shelters across New Providence, Grand Bahama, and Abaco. [59] The Ministry for Disaster Preparedness, Management, and Reconstruction in Nassau received $3.6 million-worth of modular shelters, medical evacuation boats, and construction materials from the United States embassy in ...
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September 4–5, 1965 – Hurricane Emily dissipated west of Baja California, spreading light rainfall across California of less than 1 in (25 mm). [ 3 ] : 132 August 30–31, 1967 – Hurricane Katrina produced rainfall across southern California as it traversed much of the Gulf of California, reaching over 2 in (51 mm).
California's coastal regions, the Sierra Nevada foothills, and much of the Central Valley have a Mediterranean climate, with warmer, drier weather in summer and cooler, wetter weather in winter. The influence of the ocean generally moderates temperature extremes, creating warmer winters and substantially cooler summers in coastal areas.
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