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Protected harbors such as Avalon and Two Harbors are normally sheltered and the waters within the harbors are very calm.
In strong Santa Ana conditions, these harbors develop high surf and strong winds that can tear boats from their moorings and crash them onto the shore.
As the wind narrows and is compressed into the passes its velocity increases dramatically, often to near-gale force or above.
At the same time, as the air descends from higher elevation to lower, it is heated adiabatically, warming about 5 °F for each 1,000 feet it descends (10 °C for each 1,000 m).
These low humidities, combined with the warm, compressionally-heated airmass, plus the high wind speeds, create critical fire weather conditions.
The combination of wind, heat, and dryness accompanying the Santa Ana winds turns the chaparral into explosive fuel feeding the infamous wildfires for which the region is known.
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These winds, which can easily exceed 40 miles per hour (18 m/s), are warm and dry and can severely exacerbate brush or forest fires, especially under drought conditions." This map illustration shows a characteristic high-pressure area centered over the Great Basin, with the clockwise anticyclone wind flow out of the high-pressure center giving rise to a Santa Ana wind event as the airmass flows through the passes and canyons of southern California, manifesting as a dry northeasterly wind.
During the Santa Ana winds, large ocean waves can develop.
These waves come from a northeasterly direction; toward the normally sheltered side of Catalina Island.
At night, the Santa Ana Winds merge with the land breeze blowing from land to sea and strengthen because the inland desert cools more than the ocean due to differences in the heat capacity and because there is no competing sea breeze.
Santa Ana winds often bring the lowest relative humidities of the year to coastal Southern California.