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Marine Layer Returns
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123 views7likes5:28KSBWOriginal Release: 2026-05-21

The marine layer is a cool, moist air layer that forms near the ocean surface, typically extending 750 feet in depth, which creates cooler coastal temperatures (upper 50s to mid 60s) while inland areas experience significantly warmer conditions (upper 80s to lower 90s). This temperature differential occurs because the marine layer acts as a temperature barrier, and its depth and strength directly influence daytime heating and overall weather patterns. During the afternoon and early evening, onshore winds develop due to diurnal heating differences between land and ocean, with gusts potentially reaching 30 mph. When low clouds hover near the coast, stratus clouds can spread inland through geographic features like the Golden Gate and into valleys such as the Salinas Valley.

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