Speed dating in santa ana

The air has already been dried by orographic lift before reaching the Great Basin, as well as by subsidence from the upper atmosphere, so this additional warming often causes relative humidity to fall below 10 percent.The end result is a strong, warm, and very dry wind blowing out of the bottom of mountain passes into the valleys and coastal plain.These waves come from a northeasterly direction; toward the normally sheltered side of Catalina Island.Protected harbors such as Avalon and Two Harbors are normally sheltered and the waters within the harbors are very calm.The Santa Ana winds sweep down from the deserts and across coastal Southern California, pushing dust and smoke from wild fires far out over the Pacific Ocean.

During the Santa Ana winds, large ocean waves can develop.The Santa Ana winds are strong, extremely dry down-slope winds that originate inland and affect coastal Southern California and northern Baja California.They originate from cool, dry high-pressure air masses in the Great Basin.During Santa Ana conditions it is typically hotter along the coast than in the deserts, While the Santa Anas are katabatic, they are not Föhn winds.These result from precipitation on the windward side of a mountain range which releases latent heat into the atmosphere which is then warmer on the leeward side (e.g., the Chinook or the original Föhn).

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