lomas
{{Short description|Fog-watered bioregions in the coastal desert of Peru and northern Chile}}
{{Other uses|Lomas (disambiguation)}}
{{italic title}}
Lomas (Spanish for "hills"), also called fog oases and mist oases, are areas of fog-watered vegetation in the coastal desert of Peru and northern Chile. About 100 lomas near the Pacific Ocean are identified between 5°S and 30°S latitude, a north–south distance of about {{convert|2800|km|mi}}. Lomas range in size from a small vegetated area to more than {{convert|40000|ha|acre}} and their flora includes many endemic species. Apart from river valleys and the lomas the coastal desert is almost without vegetation. Scholars have described individual lomas as "an island of vegetation in a virtual ocean of desert."Dillon, Michael O., "The Solanaceae of the Lomas Formations of Coastal Peru and Chile," www.sacha.org/solanaceae/lomas_solanaceae.pdf, accessed 17 Jul 2017
File:Lomas de Lachay.jpg is a protected area north of Lima.]]
In a nearly rainless desert, the lomas owe their existence to the moist dense fog and mist which rolls in from the Pacific. The fog is called garúa in Peru and Camanchaca in Chile.
Environment
According to the Köppen Climate Classification system, the coastal desert of Peru and the Atacama Desert of Chile feature a rare desert climate, that is abbreviated "BWn" on climate maps with the n denoting frequent fog.{{cite web |archiveurl=https://web.archive.org/web/20180122045953/http://www.gep.uchile.cl/Biodiversidad/medio_fisico/clima_01.html |archivedate=22 January 2018 |url=http://www.gep.uchile.cl/Biodiversidad/medio_fisico/clima_01.html |title=Clasificación Climática de Köppen |publisher=Universidad de Chile |language=Spanish |accessdate=21 January 2018}}{{cite web |last1=Inzunza |first1=Juan |archiveurl=https://web.archive.org/web/20180122051833/http://nimbus.com.uy/weather/Cursos/Curso_2006/Textos%20complementarios/Meteorologia%20descriptiva_Inzunza/cap15_Inzunza_Climas%20de%20Chile.pdf |archivedate=22 January 2018 |url=http://nimbus.com.uy/weather/Cursos/Curso_2006/Textos%20complementarios/Meteorologia%20descriptiva_Inzunza/cap15_Inzunza_Climas%20de%20Chile.pdf |title=Capitulo 15. Climas de Chile |work=Meteorología Descriptiva y Aplicaciones en Chile |page=427 |language=Spanish |accessdate=22 January 2018}} Temperatures are mild year round and precipitation is nearly non-existent, averaging {{convert|3|mm|inch}} to {{convert|13|mm|inch}} per year in most locations."The desert biome", http://www.ucmp.berkeley.edu/exhibits/biomes/deserts.php, accessed 16 Jul 2016 Many years have no precipitation at all. The Atacama Desert of Chile is commonly known as the driest non-polar place in the world.{{cite web|title=Yungay – the driest place in the world |url=http://www.wondermondo.com/Countries/SA/Chile/Antofagasta/Yungay.htm|work=Wondermondo |accessdate=3 April 2013 |date=3 November 2010}}{{cite book |last=Boehm |first=Richard G. |title=The World and its People |year=2005 |publisher=Glencoe/McGraw-Hill |location=New York|isbn=978-0-07-860977-0|page=276|edition=Teacher's wraparound|author2=Armstrong, David G. |author3=Hunkins, Francis P. |author4=Reinhartz, Dennis |author5= Lobrecht, Merry }}
Arica, Chile, in the middle portion of the coastal desert, went a record 173 months without measurable precipitation in the early 20th century.
Occasional rainfall is caused by El Niño. For example, in March 2015, the desert in Chile received about {{convert|25|mm|inch}} in one day which caused flooding. In a phenomenon called the flowering desert, after the rare rains the desert briefly blooms with flowers."The 'driest place on Earth' is covered with pink flowers after a crazy year of rain," The Washington Post, October 29, 2015 Normally, with the nearly non-existent precipitation, the coastal desert is almost devoid of vegetation except in lomas and along rivers which originate in the Andes and cross the desert to the Pacific.
File:A fog oasis at the Atiquipa Lomas, Peru.jpg
The moisture for the vegetation in the lomas comes from fog which rolls in from the nearby Pacific Ocean and embraces mountains which come down near the sea. The cold waters of the Humboldt Current run offshore. During the austral winter thick stratus clouds, the garúa, creep inland to an altitude of {{convert|1000|m|ft}} most days from May until November. During this season the vegetation in the lomas is lush and green and many species of flowers bloom. In the austral summer from December to April, the weather is mostly sunny and the lomas become dryer.Rundel, P. W., Dillion, M.O., Palma, B., Mooney, H.A., Gulmon, S. L., and Ehleringer, J. R., "The Phytogeography and Ecology of the Coastal Atacama and Peruvian Deserts," In Aliso. (1 ed., Vol. 13, pp. 1-49) The moisturizing impact of the fog is increased by the mild temperatures throughout the year and high average humidity of the coastal deserts. For example, Lima, Peru, located at 12°S latitude has average monthly temperatures ranging from {{convert|17|C|F}} to {{convert|23|C|F}}, very cool for locations in the tropics. Lima's average humidity is 84 percent, more than double the average humidity in most deserts."Lima, Peru. Weatherbase, http://www.weatherbase.com/weather/weather.php3?s=82648&cityname=Lima-Lima-Peru&units=metric, accessed 17 Jul 2016
File:Desert of Paracas, Peru - Paracas National Reserve.jpg
Lomas comprise less than two percent of the coastal desert areas of Chile and Peru. Peru has more than 40 lomas totaling in area less than {{convert|2000|sqkm|sqmi}} out of a total desert area of {{convert|144000|sqkm|sqmi}}. Chile has almost 50 lomas with an area of less than {{convert|5000|sqkm|sqmi}} out of a total desert area of {{convert|291000|sqkm|sqmi}}."South America, Site SA42, Lomas Formations, Peru" http://botany.si.edu/projects/cpd/sa/sa43.htm and "South America, Site SA43, Lomas Formations of the Atacama Desert, Chile", http://botany.si.edu/projects/cpd/sa/sa42.htm, accessed 16 July 2016
Climate change
Teetering on a narrow edge of survival, the lomas are sensitive to climate change. Radio-carbon dating has indicated that, prior to 3800 BCE, the Peruvian desert north of Lima (12° S latitude) received more seasonal precipitation and was mostly vegetated. Lomas—isolated fog oases—existed only south of Lima. This is evidenced by the uniformity of plant species in present-day lomas north of Lima while lomas south of Lima have more endemic plant species, indicating geographic isolation. The cause of the climatic change was probably the duration and strength of El Niño events.Quilter, Jeffrey (2014), The Ancient Central Andes, New York: Routledge, pp. 56-57
Destruction
File:Nolana elegans - Alstromeria paupercula.jpg and Alstromeria bloom in a lomas near Paposo, Chile.]]
Lomas have been impacted, and in some cases destroyed, by centuries of unregulated grazing, wood-cutting, and mining."South America, Site SA42, Lomas Formations, Peru" http://botany.si.edu/projects/cpd/sa/sa43.htm, accessed 17 July 2016 In Chile, the Huasco (28°26′ S) and Copiapó (27°22′ S) river valleys once supported dense stands of trees. In the 18th century, the city of Copiapó was known as San Francisco de la Selva (Saint Francis of the Forest) for its extensive forests.Rundel, et al, p. 14
As the branches of trees and bushes trap the fog and create more moisture for other plants, their absence reduces the viability for all the plant life in the lomas.Quilter, p. 71
In many locations the lomas were over-exploited for agriculture and grazing. One example is that, in prehistoric times, {{convert|25|km|mi}} north of Ilo, Peru, far from any other source of water, four lomas-fed springs permitted about {{convert|85|ha|acre}} of irrigated agriculture plus grazing for llamas and alpacas. Hundreds of people of the Chiribaya culture benefited from this unlikely agriculture in a rainless land. Later, during the 17th century, Spanish colonists pastured 200 mules in these lomas. As late as 1951, a few tara trees still lived although the lomas were by then nearly devoid of all vegetation and population.Zaro, Gregory (2007), "Diversity Specialists: Coastal Resource Management and Historical Contingency in the Osmore Desert of Southern Peru," Latin American Antiquity, Vol. 18, No. 2, pp. 165-174
Preservation
In Peru, the Reserva Nacional de Lachay (National Preserve of Lachay) (11°22′S) protects {{convert|5070|ha|acre}} {{convert|105|km|mile}} north of Lima."De Lachay-- Servicio Nacional de Areas Naturales Protegidas por el Estado", http://www.sernanp.gob.pe/de-lachay, accessed 17 July 2016
The Lomas de Atiquipa (15°48′S) is the largest and the best preserved lomas forest in Peru, covering more than {{convert|42000|ha|acre}} with some 350 plant species, including 44 endemics. The National University of Saint Augustine in Arequipa has partnered with Peruvian conservation groups and the Nature Conservancy to preserve and restore the environment of the lomas. Included in the project is the installation of fog-catching nets to capture water, thereby helping the 80 families who live within the area to expand agriculture, primarily of olives.Peru: The Blessing of Water in Peru's Coastal Desert," The Nature Conservancy, http://www.nature.org/ourinitiatives/regions/southamerica/peru/explore/lomas-de-atiquipa.xml {{Webarchive|url=https://web.archive.org/web/20170821173011/https://www.nature.org/ourinitiatives/regions/southamerica/peru/explore/lomas-de-atiquipa.xml |date=2017-08-21 }}, accessed 17 Jul 2016 Similar methods have been used for the conservation of lomas in Lima.{{Cite journal |last=Ojani |first=Chakad |date=2022-06-01 |title=Water in Atmospheric Suspension: Contact Zones between Ethnography and Speculative Realism |url=https://www.berghahnjournals.com/view/journals/social-analysis/66/2/sa660204.xml |journal=Social Analysis |language=en |volume=66 |issue=2 |pages=62–84 |doi=10.3167/sa.2022.660204 |issn=0155-977X|doi-access=free }}{{Cite journal |last=Ojani |first=Chakad |date=March 2023 |title=Experimenting with fog: Environmental infrastructures, infrastructuring environments, and the infrastructure of infrastructure |url=http://journals.sagepub.com/doi/10.1177/25148486221101458 |journal=Environment and Planning E: Nature and Space |language=en |volume=6 |issue=1 |pages=24–41 |doi=10.1177/25148486221101458 |s2cid=249356224 |issn=2514-8486|url-access=subscription }}{{Cite journal |last=Ojani |first=Chakad |date=June 2022 |title=Displacing (in)formality: endangered species, endangered city, and unstable grounds of comparison |journal=Journal of the Royal Anthropological Institute |language=en |volume=28 |issue=2 |pages=516–536 |doi=10.1111/1467-9655.13706 |issn=1359-0987|doi-access=free }}{{Cite journal |last=Ojani |first=Chakad |date=February 2021 |title=The (ontological) politics of fog capture in Lima, Peru |journal=Anthropology Today |language=en |volume=37 |issue=1 |pages=13–16 |doi=10.1111/1467-8322.12629 |issn=0268-540X|doi-access=free }}
In Chile the Pan de Azúcar (26°09′S) and Llanos de Challe (28°10′) National Parks and the La Chimba National Reserve (23°32′S, 70°21′W) preserve lomas. The richest diversity of species of lomas flora in Chile, however, is near the village of Paposo (25°00′S). The fog oasis near Paposo occur at elevations of {{convert|200|m|ft}} to {{convert|1000|m|ft}} with altitudes from {{convert|400|m|ft}} to {{convert|700|m|ft}} having the most abundant growth of vegetation. The Paposo area has been declared a Zone of Ecological Protection by the Government of Chile."La Flora de Quebrada de Paposo", http://www.chileflora.com/Florachilena/FloraSpanish/SHFloralPaposo.htm, accessed 18 July 2016