DescriptionMeteorologySanta Anas are a type of drainage wind, an offshore wind that results from the buildup of air pressure in the high-altitude Great Basin between the Sierra Nevada and the Rocky Mountains. When upper level winds are favorable, this high altitude air mass spills out of the Great Basin and is propelled gravitationally towards the southern California coastline, generally as a northeasterly wind. It is often said that the air is heated and dried as it passes through the Mojave and Sonoran Deserts, but according to meteorologists this is a popular misconception. The Santa Ana winds usually form during autumn and early spring when the surface air in the elevated regions of the Great Basin and Mojave Desert (the "high desert") becomes cool or even cold, although they may form at virtually any time of year. The air heats up due to adiabatic heating during its descent. While the air has already been dried by orographic lift before reaching the Great Basin as well as by subsidence from the upper atmosphere, the relative humidity of the air is further decreased as it descends from the high desert toward the coast, often falling below 10 percent. The air from the high desert is initially relatively dense owing to its coolness and aridity, and thus tends to channel down the valleys and canyons in gusts which can attain hurricane force at times. As it descends, the air not only becomes drier, but also warms adiabatically by compression. The southern California coastal region gets some of its hottest weather of the year during autumn while Santa Ana winds are blowing. During Santa Ana conditions it is typically hotter along the coast than in the deserts.
QuikSCAT image showing the speed of the Santa Ana winds (m/s).
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. Wildfires fanned by Santa Ana winds burned 721,791 acres (2,921 km²) in two weeks during October 2003.[1] These same winds have contributed to the fires that have burned some 426,000 acres as of late October 2007.[2] Although the winds often have a destructive nature, they have some positive benefits as well. They cause cold water to rise from below the surface layer of the ocean, bringing with it many nutrients that ultimately benefit local fisheries. As the winds blow over the ocean, sea surface temperatures drop about 4°C (7°F), indicating the upwelling. Chlorophyll concentrations in the surface water go from negligible, in the absence of winds, to very active at more than 1.5 milligrams per cubic meter in the presence of the winds. Santa Ana fogA Santa Ana fog is derivative phenomenon in which a ground fog settles in Southern California during the end of a Santa Ana wind episode. When Santa Ana conditions prevail, with winds in the lower two to three kilometers (1.25-1.8 m) of the atmosphere from the north through east, the lower atmosphere continues to be dry. But as soon as the Santa Ana winds cease, the cool and moist marine layer forms rapidly. The air in the marine layer becomes very moist and fog occurs.[3][4] A related phenomenon occurs when the Santa Ana condition is present but weak, allowing hot dry air to accumulate in the inland valleys that may not push all the way to sea level. Under these conditions auto commuters can drive from the San Fernando Valley where conditions are sunny and warm, over the low Santa Monica Mountains, to plunge into the cool cloudy air, low clouds, and fog characteristic of the marine air mass. This and the "Santa Ana fog" above constitute examples of an air inversion. Cold Santa Ana'sWhile characteristically hot and dry, the Santa Anas can also blow cold and dry, and in fact can bring some of Southern California's coldest weather. High cloudiness, most commonly cirrus and altostratus, but also lenticular clouds may be observed, and on rare occasions these usually dry southwest-flowing winds can bring rain. Popular experienceIn the Los Angeles Basin, the winds are often credited with the extremely high visibility experienced in the area during the winter, in contrast to the hazy, smoggy summers. The adverse pulmonary health impacts have been understood by local doctors for decades; the winds pick up and transmit grit, dust, pollens, mold spores and other irritants and allergens for considerable distances. Residents regularly notice a build-up of dust in their homes and grit on their properties during these periods, which are frequent during the winter. Similar windsTo the north, in the Santa Barbara area, the Santa Ana winds are weaker and are usually held at bay by topography: the local mountains offer no prominent outlets, in the form of passes or river valleys, from the elevated inland source areas. However, a variant of the Santa Ana wind, known locally as Sundowner winds, often invade the area. These are downslope winds which occur when a high pressure area lies due north of Santa Barbara, and occur most frequently in the late spring to early summer, and are strongest at sunset, or "sundown," hence their name. Since high pressure areas usually migrate east, changing the pressure gradient in southern California to the northeast, it is common for "sundowner" wind events to precede Santa Ana events by a day or two.[5] Winds blowing off the elevated glaciated plateaus of Greenland and Antarctica experience the most extreme form of katabatic wind, of which the Santa Ana is a type, for the most part. The winds start at a high elevation and flow outward and downslope, attaining hurricane gusts in valleys, along the shore, and even out to sea. Like the Santa Ana, these winds also heat up by compression and lose humidity, but since they start out so extraordinarily cold and dry and blow over snow and ice all the way to the sea, the perceived difference is negligible. Historical impactThe winds are also associated with some of the area's largest and deadliest wildfires, including the state's largest fire on record, the Cedar Fire, as well as the Laguna Fire, Old Fire, Esperanza Fire, Santiago Canyon Fire of 1889 and the Witch Fire. In October 2007 the winds fueled major wild fires and house burnings in Escondido, Malibu, San Marcos, Carlsbad, Rancho Bernardo, Poway, and in the major cities of San Bernardino, San Diego and Los Angeles. EtymologySanta Ana winds may get their name from the Santa Ana Mountains in Orange County, the Santa Ana River or Santa Ana Canyon, along which the winds are particularly strong. There are also claims that the original form is Santana winds, from the Spanish vientos de Satán ("winds of Satan", Sanatanas being a rarer form of Satanás), and that this, in turn, is a translation of a native name in some unspecified language.citation needed According to the Los Angeles Almanac: "The original spelling of the name of the winds is unclear, not to mention the origin. The name Santana Winds is said to be traced to Spanish California, when the winds were called devil winds due to their heat. The reference book Los Angeles A to Z (by Leonard & Dale Pitt), credits the Santa Ana Canyon in Orange County as the origin of the name Santa Ana Winds, thereby arguing for the term Santa Anas. This might be supported by early accounts which attributed the Santa Ana Riverbed running through the canyon as the source of the winds. Another account placed the origin of Santa Ana winds with an Associated Press correspondent stationed in Santa Ana who mistakenly began using Santa Ana winds instead of Santana winds in a 1901 dispatch." Santa Ana winds in popular culture
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