Wednesday, October 11, 2017

Santa Ana Winds: Wikipedia

 These are the winds usually off the desert or hotter regions when they whip out to sea and into the ocean at 40 to 100 miles per hour down canyons around mountains and to the sea in California.
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.
‎Description · ‎Related phenomena · ‎Historical impact · ‎Health effects

Santa Ana winds

From Wikipedia, the free encyclopedia
This article is about the seasonal strong winds in Southern California. For other uses, see Santa Ana winds (disambiguation).
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. Los Angeles is in the upper left of this image, and San Diego is near the center.
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.
Santa Ana winds are known for the hot dry weather that they bring in the fall (often the hottest of the year), but they can arise at other times of the year. They often bring the lowest relative humidities of the year to coastal Southern California. These low humidities, combined with the warm, compressionally-heated airmass, plus high wind speeds, create critical fire weather conditions. Known as "devil winds",[1][2] Santa Anas are infamous for fanning regional wildfires.

Contents

Description

Meteorology

The National Weather Service defines Santa Ana winds as "Strong down slope winds that blow through the mountain passes in southern California. 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."[3]
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.
The Santa Anas are katabatic winds—Greek for "flowing downhill", arising in higher altitudes and blowing down towards sea level.[4] 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 the Sierra Nevada and into the Southern California region.[5] Cool, dry air flows outward in a clockwise spiral from the high pressure center. This cool, dry airmass sweeps across 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 the coast pulls the airmass offshore.
These passes include the Soledad Pass, the Cajon Pass, and the San Gorgonio Pass, all well known for exaggerating Santa Anas as they are funneled through.[6] 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).[6] As it warms, its capacity to hold moisture increases, so its relative humidity decreases. 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.[7] 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.
During Santa Ana conditions it is typically hotter along the coast than in the deserts,[8] with the Southern California coastal region reaching some of its highest annual temperatures in autumn rather than summer.
QuikSCAT image showing the speed of the Santa Ana winds (m/s)
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 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.[7][9]

Regional Impacts

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 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. Wildfires fanned by Santa Ana winds burned 721,791 acres (2,920.98 km2) in two weeks during October 2003.[10] and another 500,000 acres (2,000 km2) in the October 2007 California wildfires.[11]
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 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.

Local maritime impacts

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. 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. During a Santa Ana, it is advised that boaters moor on the back side of the island to avoid the dangerous conditions of the front side.

Related phenomena

Santa Ana fog

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 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.[12][13] If wind gradients turn on-shore with enough strength, this sea fog is blown onto the coastal areas. This marks 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 envelope 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, 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 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.

Sundowner winds

The similar winds in the Santa Barbara 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.[14]

Arctic and Antarctic katabatic winds

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 because they start out so extraordinarily cold and dry and blow over snow and ice all the way to the sea, the perceived similarity is negligible.

Historical impact

The Santa Ana winds and 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.[15]
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.[1] 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 the Los Angeles Basin was primarily an agricultural region, the winds were feared particularly by farmers for their potential to destroy crops.[1]
The 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 Creek Fire.
In October 2007, the winds fueled major wild fires and house burnings in Escondido, Malibu, Rainbow, San Marcos, Carlsbad, Rancho Bernardo, Poway, Ramona, and in the major cities of San Bernardino, San Diego and Los Angeles. The Santa Ana winds were also a factor in the November 2008 California wildfires.
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 110 MPH sustained winds and 170 MPH gusts (unconfirmed).[16] The winds toppled thousands of trees, knocking out power for over 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.[17] The winds also ripped through Mammoth Mountain and parts of Utah. Mammoth Mountain holds California's highest wind gust of 175 MPH from that night.
In May 2014, the Santa Ana winds initiated the May 2014 San Diego County wildfires, approximately four months after the Colby Fire in northern Los Angeles County.

Health effects

Especially hot, dry, and dusty Santa Ana winds are widely believed (in Southern California, at least) to affect people's moods and behavior negatively. This has not been definitively proven in studies, although limited evidence may point to this conclusion.[18] Even without ironclad scientific proof, it is a well-accepted part of local lore.[2]
The winds carry Coccidioides immitis and Coccidioides posadasii spores into nonendemic areas,[19][20] 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).[21] Serious complications include severe pneumonia, lung nodules, and disseminated disease, where the fungus spreads throughout the body. The disseminated form of Coccidioidomycosis can devastate the body, causing skin ulcers, abscesses, bone lesions, severe joint pain, heart inflammation, urinary tract problems, meningitis, and often death.[22]
There is some belief the winds also create positive ions, which are believed to affect mood negatively. Many believe this to be the cause for the statistical increase in the number of suicides and homicides during these times.[2][23][24][25][26][27]

Etymology

The most well-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 the winds blow intensely.[1][4] Newspaper references to the name Santa Ana winds date as far back as 1880.
Another attempt at explanation of the name claims that it derives from a Native American term for "devil wind" that was altered by the Spanish into the form "Satanás" (meaning Satan), and then later corrupted by the Catholic Church (wanting nothing to do with the Devil or "Satan") into "Santa Ana." Another derivation cited by a late KABC television meteorologist, Dr. George Fischbeck, cited the etymology of the Santana winds as coming from the early Mexicano/Angeleno: "Caliente aliento de Satanás" or "hot breath of Satan."

In popular culture

Main article: Santa Ana winds in popular culture
The Santa Ana winds are commonly portrayed in fiction as being responsible for a tense, uneasy, wrathful mood among Angelenos. Some of the more well-known literary references include the Philip Marlowe story "Red Wind" by Raymond Chandler, and Joan Didion's Slouching Towards Bethlehem.[1][2]

See also

References


  • Masters, Nathan (October 25, 2012). "SoCal's Devil Winds: The Santa Anas in Historical Photos and Literature". www.kcet.org. KCET. Retrieved May 3, 2012. "(White)Scholars who have looked into the name's origins generally agree that it derives from Santa Ana Canyon, the portal where the Santa Ana River -- as well as a congested Riverside (CA-91) Freeway -- leaves Riverside County and enters Orange County. When the Santa Anas blow, winds can reach exceptional speeds in this narrow gap between the Puente Hills and Santa Ana Mountains."
    1. The Gazette - Mar 30, 1999 The positive ions created by the winds may make people more irritable, anxious and aggressive. When Southern California's hot, dry Santa Ana winds blow into

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  • Needham, John (March 12, 1988). "The Devil Winds Made Me Do It : Santa Anas Are Enough to Make Anyone's Hair Stand on End". www.latimes.com. Los Angeles Times. Retrieved May 3, 2013.

  • "Santa Ana Wind". NOAA's National Weather Service Glossary. NOAA National Weather Service. Retrieved 10 February 2011.

  • Fovell, Robert. "UCLA explains the naming of the Santa Ana winds". http://sciencedude.blog.ocregister.com/. Orange County Register. Archived from the original on May 25, 2017. Retrieved May 3, 2012. External link in |website= (help)

  • "Santa Ana". cnap.ucsd.edu. California Nevada Applications Program / California Climate Change Center. October 3, 2015. Retrieved October 30, 2015.

  • "What are the Santana or Santa Ana Winds?". www.laalmanac.com. Los Angeles Almanac. Retrieved October 30, 2015.

  • Fovell. "The Santa Ana Winds". UCLA. Retrieved 22 November 2015.

  • "Santa Ana Winds - Wildfires". NOAA Watch All Hazards Monitor. NOAA National Weather Service. Retrieved 10 February 2011.

  • Leneman, Mike (2015). "Devil winds: Santa Ana Winds explained by one of us". The Mariner. Pat Reynolds. Nov 2015 (153): 8–9. Retrieved 22 November 2015.

  • *http://www.geotimes.org/oct03/WebExtra103103.html

  • Fire deaths, damage come into focus as evacuees cope

  • Leipper, D. F., Fog development at San Diego, California, J. Mar. Research, 7, 337-346, 1948.

  • Leipper, D. F., Fog on the United States West Coast: a review. Bull. Amer. Meteor. Soc. 75, 229-240.

  • Ryan, G., and L. E. Burch, 1992: An analysis of sundowner winds: A California downslope wind event. Preprints, Sixth Conf. on Mountain Meteorology, Portland, OR, Amer. Meteor. Soc., 64-67.

  • Rutten, Tim (October 15, 2000). "L.A., land of fire -- always". latimes.com. Los Angeles Times. Retrieved May 3, 2013.

  • https://www.wunderground.com/blog/weatherhistorian/big-winds-in-the-west-possible-wind-gust-record-in-california

  • https://www.nytimes.com/2011/12/02/us/santa-ana-winds-buffet-california.html?_r=0

  • Studying the Dust Kicked up by the Santa Anas

  • "COCCIDIOIDOMYCOSIS" (PDF). Department of Public Health. Retrieved 2014-01-19.

  • Lawrence L. Schmelzer, M.P.H.; Irving R. Tabershaw, M.D., F.A.P.H.A. (1968). Exposure Factors In Occupational Coccidioidomycosis. McGraw Hill. p. 110.

  • Ryan KJ; Ray CG (editors) (2004). Sherris Medical Microbiology (4th ed.). McGraw Hill. pp. 680–83. ISBN 0-8385-8529-9.

  • "Coccidioidomycosis". Merck. Retrieved 2014-01-19.

  • 'Human Barometer' Physicist Probes Heat Moods of Man The Windsor Star - Nov 13, 1962

  • McGinnis, Judith. "McGinnis: Ion the coif". Times Record News. Retrieved 2011-11-27.

  • Los Angeles Times, Oct 25, 1964, Santa Ana winds that bleach and burn Southern California descend through ... ratio of positive ions to negative ions in the air is greater than normal.

  • Los Angeles Times - Mar 12, 1988 "Negative ions make us feel good, positive ions make us feel badly," [Paul Blair ] said. Daily News of Los Angeles : SANTA ANAS: ILL WINDS THAT BLOW...

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