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46-496: The Santa Ana winds , also sometimes called the devil winds , are strong, extremely dry downslope 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 . Santa Ana winds are known for the hot, dry weather that they bring in autumn (often the hottest of the year), but they can also arise at other times of

92-546: A "strange, dust-laden windstorm" arrived in the night while his troops were marching south through California in January 1847. Various episodes of hot, dry winds have been described over this history as dust storms, hurricane-force winds, and violent north-easters, damaging houses and destroying fruit orchards. Newspaper archives have many photographs of regional damage dating back to the beginnings of news reporting in Los Angeles. When

138-460: A few regions of continental Antarctica the snow is scoured away by the force of the katabatic winds, leading to "dry valleys" (or " Antarctic oases ") such as the McMurdo Dry Valleys . Since the katabatic winds are descending, they tend to have a low relative humidity, which desiccates the region. Other regions may have a similar but lesser effect, leading to "blue ice" areas where the snow

184-564: A full glass of beer at a cocktail lounge. The baby frets. The maid sulks. I rekindle a waning argument with the telephone company, then cut my losses and lie down, given over to whatever is in the air. To live with the Santa Ana is to accept, consciously or unconsciously, a deeply mechanistic view of human behavior. ... [T]he violence and the unpredictability of the Santa Ana affect the entire quality of life in Los Angeles, accentuate its impermanence, its unreliability. The wind shows us how close to

230-415: A pathogenic fungus that causes Coccidioidomycosis ("Valley Fever"). Symptomatic infection (40 percent of cases) usually presents as an influenza-like illness with fever, cough, headaches, rash, and myalgia (muscle pain). Serious complications include severe pneumonia, lung nodules, and disseminated disease, where the fungus spreads throughout the body. The disseminated form of Coccidioidomycosis can devastate

276-452: A plateau, a mountain, glacier, or even a hill. Since the density of air is inversely proportional to temperature , the air will flow downwards, warming approximately adiabatically as it descends. The temperature of the air depends on the temperature in the source region and the amount of descent. In the case of the Santa Ana , for example, the wind can (but does not always) become hot by

322-578: A stable air mass is carried over the mountain by strong winds that increase in strength with height. Moisture is removed and latent heat released as the air mass is orographically lifted. As the air mass descends, it is compression heated. The warm foehn wind , locally known as the Chinook wind , Bergwind or Diablo wind or Nor'wester depending on the region, provide examples of this type of wind, and are driven in part by latent heat released by orographic-lifting-induced precipitation. A similar class of winds,

368-410: A strong correlation with the highest "regionally averaged" wind speeds. Santa Ana winds often bring the lowest relative humidities of the year to coastal Southern California. These low humidities, combined with the warm, compressionally-heated air mass , plus the high wind speeds, create critical fire weather conditions. The combination of wind, heat, and dryness accompanying the Santa Ana winds turns

414-423: A sudden and surprising transition from the hot, dry Santa Ana conditions to cool, moist, and gray marine weather, as the Santa Ana fog can blow onshore and envelop cities in as quickly as fifteen minutes. However, a true Santa Ana fog is rare, because it requires conditions conducive to rapid re-forming of the marine layer, plus a rapid and strong reversal in wind gradients from off-shore to on-shore winds. More often,

460-431: A week. Schools were closed, and a "state of emergency" was declared. The winds grounded planes at LAX, destroyed homes, and were even strong enough to snap a concrete stop light from its foundation. The winds also ripped through Mammoth Mountain and parts of Utah. Mammoth Mountain experienced a near-record wind gust of 175 mph (282 km/h), on December 1, 2011. Because they are simultaneous "gusty" and "desiccating,"

506-608: Is a strong, warm, and very dry wind blowing out of the bottom of mountain passes into the valleys and coastal plain. These warm, dry winds, which can easily exceed 40 miles per hour (64 km/h), can severely exacerbate brush or forest fires, especially under drought conditions. During Santa Ana conditions it is typically hotter along the coast than in the deserts, with the Southern California coastal region reaching some of its highest annual temperatures in autumn rather than summer. Frigid, dry arctic air from Canada tends to create

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552-459: Is advised that boaters moor on the Southern side of affected islands or return to the mainland. A Santa Ana fog is a derivative phenomenon in which a ground fog settles in coastal Southern California at 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 miles) of the atmosphere from the north through east, the air over

598-552: Is likely a false etymology . In 1933, Father John O'Connell of Mission San Juan Capistrano reported that Don Jesus Aguilar, born 1855 at Capistrano, said that in his day the winds had been called el viento del norte . Santa Ana winds are widely believed to affect people's moods and behavior. The Santa Ana winds are commonly portrayed in fiction as being responsible for a tense, uneasy, wrathful mood among Angelenos. As The New York Times put it in 2003, "a dry, hot Santa Ana often symbolizes an unnamable menace lying just beneath

644-714: Is removed and the surface ice sublimates , but is replenished by glacier flow from upstream. In the Fuegian Archipelago ( Tierra del Fuego ) in South America as well as in Alaska in North America, a wind known as a williwaw is a particular danger to harboring vessels. Williwaws originate in the snow and ice fields of the coastal mountains, and they can be faster than 120 kn (220 km/h; 140 mph). In California, strong katabatic wind events have been responsible for

690-535: The Riverside Press-Enterprise in 2020: According to research done by Orange County historian Chris Jepsen, the first reported reference to that term comes to us in 1871 from the Anaheim Gazette . To anyone in what would become Orange County at the time, the winds seem to come out of Santa Ana Canyon, hence the name. However, having Santa Ana winds named for their city did not please the members of

736-456: The Santa Barbara and Goleta area occur most frequently in the late spring to early summer, and are strongest at sunset, or "sundown"; hence their name: sundowner. Because 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. The Santa Ana winds and

782-583: The Sierra Nevada and into the Southern California region. According to one meteorology journal, "a popular rule of thumb used by forecasters is to measure the difference in pressure between the Los Angeles International Airport and Las Vegas ; a difference of 9 millibars (0.27 inches of mercury ) is enough to support a Santa Ana event." Dry air flows outward in a clockwise spiral from the high pressure center. This dry airmass sweeps across

828-848: The bora in the Adriatic , the Bohemian Wind or Böhmwind in the Ore Mountains , the Santa Ana in southern California , the piteraq winds of Greenland, and the oroshi in Japan . Another example is "the Barber", an enhanced katabatic wind that blows over the town of Greymouth in New Zealand when there is a southeast flow over the South Island. "The Barber" has a local reputation for its coldness. A katabatic wind originates from radiational cooling of air atop

874-431: The chaparral into explosive fuel feeding the infamous wildfires for which the region is known. Although the winds often have a destructive nature, they have some 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

920-686: 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. During the Santa Ana winds, large ocean waves can develop. These waves come from a northeasterly direction toward the normally sheltered sides of the Channel Islands , including commonly visited Catalina and Santa Cruz islands. Normally well-sheltered harbors and anchorages such as Avalon and Two Harbors can develop high surf and strong winds that can tear boats from their moorings. During Santa Ana conditions, it

966-691: The Chamber of Commerce in the city of Santa Ana , and they fought for years to get the name changed. The name Santa Ana wind became nationally known following a sensationalized 1901 wire story about wind damage. One narrative claimed that the term Santa Ana wind derives from a Native American phrase for "devil wind" that was then altered by Californios into the form "Satanás" (meaning Satan ), and then still later corrupted into "Santa Ana". However, an authority on local Native American languages claims this supposed Indigenous term "Santana" never existed. No evidence has ever emerged to support this explanation and it

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1012-630: The Los Angeles Basin was primarily an agricultural region, the winds were feared particularly by farmers for their potential to destroy crops. In early December 2011, the Santa Ana winds were the strongest yet recorded. An atmospheric set-up occurred that allowed the towns of Pasadena and Altadena in the San Gabriel Valley to get whipped by sustained winds at 97 mph (156 km/h), and gusts up to 167 mph (269 km/h). The winds toppled thousands of trees, knocking out power for over

1058-573: The Pacific Coast around Los Angeles from inland desert regions". Santa Ana winds originate from high-pressure airmasses over the Great Basin and upper Mojave Desert. Any low-pressure area over the Pacific Ocean, off the coast of California, can change the stability of the Great Basin High, causing a pressure gradient that turns the synoptic scale winds southward down the eastern side of

1104-486: The Santa Ana starts to blow, I invariably grow edgy...unable, in the most concrete sense, to settle myself down." There was a desert wind blowing that night. It was one of those hot dry Santa Anas that come down through the mountain passes and curl your hair and make your nerves jump and your skin itch. On nights like that every booze party ends in a fight. Meek little wives feel the edge of the carving knife and study their husbands' necks. Anything can happen. You can even get

1150-646: The Santa Ana winds are highly associated with regional wildfire danger. The winds have been implicated in some of the area's (and even the state's) largest and deadliest wildfires , including the Thomas Fire , and Cedar Fire , as well as the Laguna Fire , Old Fire , Esperanza Fire , and the Witch Creek Fire . Other major wildfires fueled by Santa Ana winds include: The winds carry Coccidioides immitis and Coccidioides posadasii spores into nonendemic areas,

1196-625: The accompanying raging wildfires have been a part of the ecosystem of the Los Angeles Basin for over 5,000 years, dating back to the earliest habitation of the region by the Tongva and Tataviam peoples. The Santa Ana winds have been recognized and reported in English-language records as a weather phenomenon in Southern California since at least the mid-nineteenth century. During the Mexican–American War , Commodore Robert Stockton reported that

1242-534: The body, causing skin ulcers, abscesses, bone lesions, severe joint pain, heart inflammation, urinary tract problems, meningitis, and often death. The best-accepted explanation for the name Santa Ana winds is that it is derived from the Santa Ana Canyon in Orange County , one of the many locations where the winds blow intensely. Newspaper references to the name Santa Ana winds appear as far back as 1882. Per

1288-593: The coast pulls the airmass offshore. Mountain passes which channel these winds include the Soledad Pass , the Cajon Pass , and the San Gorgonio Pass , all well known for exaggerating Santa Anas as they are funneled through. 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,

1334-426: The coastal basin is extremely dry, and this dry air extends out over offshore waters of the Pacific Ocean. When the Santa Ana winds cease, the cool and moist marine layer may re-form rapidly over the ocean if conditions are right. The air in the marine layer becomes very moist and very low clouds or fog occurs. If wind gradients turn on-shore with enough strength, this sea fog is blown onto the coastal areas. This marks

1380-495: The day because the strong offshore desert winds oppose the on-shore sea breeze. 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 are associated in the public mind with dry hot weather, but cold Santa Anas not only exist but have

1426-453: The deserts of eastern California toward the coast, and encounters the towering Transverse Ranges , which separate coastal Southern California from the deserts. The airmass, flowing from high pressure in the Great Basin to a low pressure center off the coast, takes the path of least resistance by channeling through the mountain passes to the lower coastal elevations, as the low pressure area off

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1472-434: The edge we are. When the hills of Los Angeles are burning Palm trees are candles in the murder winds So many lives are on the breeze/ Even the stars are ill at ease And Los Angeles is burning. Some of this experienced mood shift is likely due to the increase of static electricity in dry conditions. California folklore therefore credits the winds with "strange luminosity in the form of sparks and glows that accompany

1518-416: The explosive growth of many wildfires, including the 2018 Camp Fire and the 2020 North Complex . Orographic lift Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain . As the air mass gains altitude it quickly cools down adiabatically , which can raise the relative humidity to 100% and create clouds and, under

1564-509: The high pressure system over the Great Basin, which caused the Santa Ana conditions in the first place, is slow to weaken or move east across the United States. In this more usual case, the Santa Ana winds cease, but warm, dry conditions under a stationary air mass continue for days or even weeks after the Santa Ana wind event ends. A related phenomenon occurs when the Santa Ana condition is present but weak, allowing hot dry air to accumulate in

1610-406: The ice sheets and the elevation of the ice sheets brings into play enormous gravitational energy. Where these winds are concentrated into restricted areas in the coastal valleys, the winds blow well over hurricane force, reaching around 160 kn (300 km/h; 180 mph). In Greenland these winds are called piteraq and are most intense whenever a low pressure area approaches the coast. In

1656-471: 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 . The similar winds in

1702-460: The most intense Santa Ana winds. 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). If the Santa Anas are strong, the usual day-time sea breeze may not arise, or develop weak later in

1748-432: The right conditions, precipitation . Orographic lifting can have a number of effects, including precipitation, rain shadowing, leeward winds, and associated clouds. Precipitation induced by orographic lift occurs in many places throughout the world . Examples include: The highest precipitation amounts are found slightly upwind from the prevailing winds at the crests of mountain ranges, where they relieve and therefore

1794-970: The sun-shot surface of California life." According to the Pasadena Public Library  [ Wikidata ] book blog, the winds notably appear in Richard Henry Dana 's Two Years Before the Mast , the Philip Marlowe story "Red Wind" by Raymond Chandler , three essays by Joan Didion about Los Angeles, ("Los Angeles Notebook" and "Some Dreamers of the Golden Dream", both included in her 1968 book Slouching Towards Bethlehem , and "Fire Season", included in her 1992 book After Henry ), The Husband by Dean Koontz , White Oleander by Janet Fitch , and Less than Zero by Bret Easton Ellis . In Thomas Pynchon 's 2009 "California novel" Inherent Vice

1840-459: The temperature and barometric pressure increase adiabatically , warming about 5 °F for each 1,000 feet it descends (1 °C for each 100 m). Relative humidity decreases with the increasing temperature. 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

1886-473: The time it reaches sea level. In Antarctica, by contrast, the wind is still intensely cold. The entire near-surface wind field over Antarctica is largely determined by the katabatic winds, particularly outside the summer season, except in coastal regions when storms may impose their own wind field. Katabatic winds are most commonly found blowing out from the large and elevated ice sheets of Antarctica and Greenland . The buildup of high density cold air over

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1932-436: The upward lifting is greatest. As the air descends the lee side of the mountain, it warms and dries, creating a rain shadow. On the lee side of the mountains, sometimes as little as 15 miles (25 km) away from high precipitation zones, annual precipitation can be as low as 8 inches (200 mm) per year. Areas where this effect is observed include: Downslope winds occur on the leeward side of mountain barriers when

1978-418: The winds make an appearance and, per one scholar, "the obligatory noir description of their effects appears on page 98." Los Angeles Times columnist David L. Ulin commented, "...for writers such as Didion and Chandler, the Santa Ana is an emblem of disruption because, for them, Los Angeles is a disrupted world. We can take issue with that impression of the city; I sometimes do and sometimes don't. But when

2024-406: The winds" and an excess of "positive ions , disrupting health, well-being, and temperament." Katabatic wind Not all downslope winds are katabatic. For instance, winds such as the föhn and chinook are rain shadow winds where air driven upslope on the windward side of a mountain range drops its moisture and descends leeward drier and warmer. Examples of true katabatic winds include

2070-506: The year. They often bring the lowest relative humidities of the year to coastal Southern California, and "beautifully clear skies". These low humidities, combined with the warm, compressionally-heated air mass, plus high wind speeds, create critical fire weather conditions and fan destructive wildfires . Typically, about 10 to 25 Santa Ana wind events occur annually. A Santa Ana can blow from one to seven days, with an average wind event lasting three days. The longest recorded Santa Ana event

2116-999: Was a 14-day wind in November 1957. Damage from high winds is most common along the Santa Ana River basin in Orange County, the Santa Clara River basin in Ventura and Los Angeles County , through Newhall Pass into the San Fernando Valley of Los Angeles County, and through the Cajon Pass into San Bernardino County near San Bernardino , Fontana , and Chino . The Santa Anas are katabatic winds (Greek for "flowing downhill") arising in higher altitudes and blowing down towards sea level. The National Weather Service defines Santa Ana winds as "a weather condition [in southern California] in which strong, hot, dust-bearing winds descend to

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