Jump to content

El Niño

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by 64.107.152.2 (talk) at 18:56, 1 April 2009 (→Wider effects of El Niño conditions). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

For other uses, see El Niño (disambiguation).
Average circulation in the south Pacific Ocean

El Niño-Southern Oscillation (ENSO; commonly referred to as simply El Niño) is a global coupled ocean-atmosphere phenomenon. The Pacific ocean signatures, El Niño and La Niña are important temperature fluctuations in surface waters of the tropical Eastern Pacific Ocean. The name El Niño, from the Spanish for "the little boy", refers to the Christ child, because the phenomenon is usually noticed around Christmastime in the Pacific Ocean off the west coast of South America.[1] La Niña, similarly, means "the little girl". These effects were first described in 1923 by Sir Gilbert Thomas Walker from whom the Walker circulation, an important aspect of the Pacific ENSO phenomenon, takes its name. The atmospheric signature, the Southern Oscillation (SO) reflects the monthly or seasonal fluctuations in the air pressure difference between Tahiti and Darwin, Australia. The most recent occurrence of El Niño started in September 2006[2] and lasted until early 2007.[3] From June 2007 on, data indicated a weak La Niña event, strengthening in early 2008 and weakening in late 2008, with a forecast return to neutral conditions in 2009.

ENSO is associated with floods, droughts, and other disturbances in a range of locations around the world. These effects, and the irregularity of the ENSO phenomenon, makes predicting it of high interest. Significant advances in the predictability of ENSO were contributed by Stephen Zebiak and Mark Cane.[4] ENSO is the most prominent known source of inter-annual variability in weather and climate around the world (about 3 to 8 years), though not all areas are affected. ENSO has signatures in the Pacific, Atlantic and Indian Oceans.

During major warm events, El Niño warming extends over much of the tropical Pacific and becomes clearly linked to the intensity of the Southern Oscillation. While ENSO effects are basically in phase between the Pacific and Indian Oceans, ENSO effects in the Atlantic Ocean lag behind those in the Pacific by 12 to 18 months. Many of the countries most affected by ENSO are developing countries that are largely dependent upon their agricultural and fishery sectors for food supply, employment, and foreign exchange.

New capabilities to predict the onset of ENSO events can have global socio-economic impacts. While ENSO is a natural part of the Earth's climate, an important concern is whether its intensity or frequency may change as a result of global warming. Low-frequency variability has been evidenced; interdecadal modulation of ENSO from the Pacific Decadal Oscillation (PDO) or the Interdecadal Pacific Oscillation (IPO) might exist. This could explain the so-called protracted ENSO of the early 1990s.

El Niño and La Niña

Normal Pacific pattern. Equatorial winds gather warm water pool toward west. Cold water upwells along South American coast. (NOAA / PMEL / TAO)
El Niño Conditions. Warm water pool approaches South American coast. Absence of cold upwelling increases warming.
La Niña Conditions. Warm water is further west than usual.

El Niño and La Niña are officially defined as sustained sea surface temperature anomalies of magnitude greater than 0.5°C across the central tropical Pacific Ocean. When the condition is met for a period of less than five months, it is classified as El Niño or La Niña conditions; if the anomaly persists for five months or longer, it is classified as an El Niño or La Niña episode. Historically, it has occurred at irregular intervals of 2-7 years and has usually lasted one or two years.

The first signs of an El Niño are:

  1. Rise in air pressure over the Indian Ocean, Indonesia, and Australia
  2. Fall in air pressure over Tahiti and the rest of the central and eastern Pacific Ocean
  3. Trade winds in the south Pacific weaken or head east
  4. Warm air rises near Peru, causing rain in the northern Peruvian deserts
  5. Warm water spreads from the west Pacific and the Indian Ocean to the east Pacific. It takes the rain with it, causing extensive drought in the western Pacific and rainfall in the normally dry eastern Pacific.

El Niño's warm current of nutrient-poor tropical water, heated by its eastward passage in the Equatorial Current, replaces the cold, nutrient-rich surface water of the Humboldt Current, also known as the Peru Current, which support great populations of food fish. In most years the warming lasts only a few weeks or a month, after which the weather patterns return to normal and fishing improves. However, when El Niño conditions last for many months, more extensive ocean warming occurs and its economic impact to local fishing for an international market can be serious.

During non-El Niño conditions, the Walker circulation is seen at the surface as easterly trade winds which move water and air warmed by the sun towards the west. This also creates ocean upwelling off the coasts of Peru and Ecuador and brings nutrient-rich cold water to the surface, increasing fishing stocks. The western side of the equatorial Pacific is characterized by warm, wet low pressure weather as the collected moisture is dumped in the form of typhoons and thunderstorms. The ocean is some 60 cm higher in the western Pacific as the result of this motion.[5][6][7][8]

In the Pacific, La Niña is characterized by unusually cold ocean temperatures in the eastern equatorial Pacific, compared to El Niño, which is characterized by unusually warm ocean temperatures in the same area. Atlantic tropical cyclone activity is generally enhanced during La Niña. The La Niña condition often follows the El Niño, especially when the latter is strong.

Regional impacts of warm ENSO episodes (El Niño).
Regional impacts of cold ENSO episodes. (La Niña)

Wider effects of El Niño conditions

See also: Effects of the El Niño-Southern Oscillation in the United States

Because El Niño's warm pool feeds thunderstorms above, it creates increased rainfall across the east-central and eastern Pacific Ocean.

The effects of El Niño in South America are direct and stronger than in North America. An El Niño is associated with warm and very wet summers (December-February) along the coasts of northern Peru and Ecuador, causing major flooding whenever the event is strong or extreme. The effects during the months of February, March and April may become critical. Southern Brazil and northern Argentina also experience wetter than normal conditions but mainly during the spring and early summer. Central Chile receives a mild winter with large rainfall, and the Peruvian-Bolivian Altiplano is sometimes exposed to unusual winter snowfall events. Drier and hotter weather occurs in parts of the Amazon River Basin, Colombia and Central America big nose america.

Direct effects of El Niño resulting in drier conditions occur in parts of Southeast Asia and Northern Australia, increasing bush fires and worsening haze and decreasing air quality dramatically. Drier than normal conditions are also generally observed in Queensland, inland Victoria, inland New South Wales and eastern Tasmania from June to August.

West of the Antarctic Peninsula, the Ross, Bellingshausen, and Amundsen Sea sectors have more sea ice during El Niño. The latter two and the Weddell Sea also become warmer and have higher atmospheric pressure.

In North America, typically, winters are warmer than normal in the upper Midwest states, the Northeast, and Canada, while central and southern California, northwest Mexico and the southwestern U.S., are wetter and cooler than normal. Summer is wetter in the intermountain regions of the U.S. The Pacific Northwest states, on the other hand, tend to experience dry but foggy winters and warm, sunny and precocious springs during an El Niño. During a La Niña, by contrast, the Midwestern U.S. tends to be drier than normal. El Niño is associated with increased wave caused coastal erosion along the US Pacific Coast and decreased hurricane activity in the Atlantic, especially south of 25º N; this reduction is largely due to stronger wind shear in the tropics.

Finally, East Africa, including Kenya, Tanzania and the White Nile basin experiences, in the long rains from March to May, wetter than normal conditions. There also are drier than normal conditions from December to February in south-central Africa, mainly in Zambia, Zimbabwe, Mozambique and Botswana.

Western Hemisphere Warm Pool

Study of climate records has found that about half of the summers after an El Niño have unusual warming in the Western Hemisphere Warm Pool (WHWP). This affects weather in the area and seems to be related to the North Atlantic Oscillation.

Atlantic effect

An effect similar to El Niño sometimes takes place in the Atlantic Ocean, where water along equatorial Africa's Gulf of Guinea becomes warmer and eastern Brazil becomes cooler and drier. This is related to El Niño's effect on the Walker circulation over South America, which causes the easterly trade winds in the western Atlantic Ocean region to strengthen.

Cases of double El Niño events have been linked to severe famines related to the extended failure of monsoon rains, as in the book Late Victorian Holocausts.

Non-climate effects

Along the west coast of South America, El Niño reduces the upwelling of cold, nutrient-rich water that sustains large fish populations, which in turn sustain abundant sea birds, whose droppings support the fertilizer industry.

East Pacific fishing

The local fishing industry along the affected coastline can suffer during long-lasting El Niño events. The world's largest fishery collapsed due to overfishing during the 1972 El Niño Peruvian anchoveta reduction. During the 1982-83 event, jack mackerel and anchoveta populations were reduced, scallops increased in warmer water, but hake followed cooler water down the continental slope, while shrimp and sardines moved southward so some catches decreased while others increased.[9] Horse mackerel have increased in the region during warm events.

Shifting locations and types of fish due to changing conditions provide challenges for fishing industries. Peruvian sardines have moved during El Niño events to Chilean areas. Other conditions provide further complications, such as the government of Chile in 1991 creating restrictions on the fishing areas for self-employed fishermen and industrial fleets.

The ENSO variability may contribute to the great success of small fast-growing species along the Peruvian coast, as periods of low population removes predators in the area. Similar effects benefit migratory birds which travel each spring from predator-rich tropical areas to distant winter-stressed nesting areas. There is some evidence that El Niño activity is correlated with incidence of red tides off the Pacific coast of California.

It has been postulated that a strong El Niño led to the demise of the Moche and other pre-Columbian Peruvian cultures.

A recent study of El Niño patterns suggests that the French Revolution was caused in part by the poor crop yields of 1788-89 in Europe, resulting from an unusually strong El-Niño effect between 1789-93.[10]

La Niña

Sea surface skin temperature anomalies in November 2007 showing La Niña conditions

La Niña is the name for the cold phase of ENSO, during which the cold pool in the eastern Pacific intensifies and the trade winds strengthen. The name La Niña originates from Spanish, meaning "the little girl", analogous to El Niño meaning "the little boy". It has also in the past been called anti-El Niño.

Effects of La Niña

Regional impacts of La Niña.

La Niña causes mostly the opposite effects of El Niño, for example, El Niño would cause a wet period in the Midwestern U.S., while La Niña would typically cause a dry period in this area.

Recent occurrences

There was a strong La Niña episode during 1988-1989. La Niña also formed in 1995, and in 1999-2000. The last La Niña was a minor one, and occurred 2000-2001. Recently, there was a moderate La Niña, which began developing in mid-2007.The NOAA confirmed that a moderate La Niña developed in their November El Niño/Southern Oscillation Diagnostic Discussion, and that it will likely continue into 2008. According to NOAA, "Expected La Niña impacts during November – January include a continuation of above-average precipitation over Indonesia and below-average precipitation over the central equatorial Pacific. For the contiguous United States, potential impacts include above average precipitation in the Northern Rockies, Northern California, and in southern and eastern regions of the Pacific Northwest. Below-average precipitation is expected across the southern tier, particularly in the southwestern and southeastern states."[11] In March 2008, La Niña caused a drop in sea surface temperatures over Southeast Asia by an amount of 2°C. It also caused heavy rains over Malaysia, Singapore and Indonesia.[12]

ENSO and global warming

A few years ago, attribution of recent changes (if any) in ENSO or predictions of future changes were very weak.[13] More recent results tend to suggest that the projected tropical warming may follow a somewhat El Niño-like spatial pattern, without necessarily altering the variability about this pattern,[14] while the ENSO cycle may be minimally shortened.[15]

Causes of El Niño

The mechanisms that cause an El Niño event are still being investigated due to the difficulties in establishing clear patterns that allow reliable forecasts. As the phenomenon is located near the equator, events in both hemispheres may have an effect, and since weather events (made up of changeable wind directions) show some chaotic tendencies, the onset of El Niño-events reflects this. Long-range forecasts remain tentative for this reason.

Major theories

  • Jacob Bjerknes in 1969 suggested that an anomalously warm spot in the eastern Pacific can weaken the east-west temperature difference, causing weakening in the Walker circulation and trade wind flows, which push warm water to the west. The result is increasingly warm water toward the east.
  • Wyrtki in 1975 proposed that increased trade winds could build up the western bulge of warm water, and any sudden weakening in the winds would allow that warm water to surge eastward. However, there was no such buildup preceding the 1982-83 event.
  • Recharge oscillator: Several mechanisms have been proposed where warmth builds up in the equatorial area, then is dispersed to higher latitudes by an El Niño event. The cooler area then has to "recharge" warmth for several years before another event can take place.
  • Western Pacific oscillator: In the western Pacific, several weather conditions can cause westerly wind anomalies. For example, cyclones north and south of the equator force west-to-east winds between. Such wind may counteract the typical easterly flows across the Pacific and create a tendency toward continuing the eastward motion. A weakening in the westward currents at such a time may be the final trigger needed to shift into an El Niño.
  • Equatorial Pacific Ocean may tend to be near El Niño conditions, with several random variations affecting behavior. Weather patterns from outside the area or volcanic events may be some such factors.
  • The Madden-Julian Oscillation (MJO) is an important source of variability that can contribute to a more rapid evolution toward El Niño conditions through related fluctuations in low-level winds and precipitation over the western and central equatorial Pacific. Eastward-propagating oceanic Kelvin waves can be produced by MJO activity. The MJO may in turn be influenced by a developing El Niño, leading to a positive feedback.[16]
  • Adams, Mann and Ammann, using statistical analysis of paleoclimatic records, that a volcanic event in the tropics tilts the climate into a state where El Niño-like conditions are favored. (This is caused by the volcano's effect on solar radiation reaching the surface, not by the heat of the eruption itself.)[17]
  • Australian geologist Ian Plimer has stated that El Niño is caused by earthquake activity and volcanic activity in the mid-ocean ridges.[18]

History of the theory

The first mention of the term "El Niño" to refer to climate occurs in 1892, when Captain Camilo Carrillo told the Geographical society congress in Lima that Peruvian sailors named the warm northerly current "El Niño" because it was most noticeable around Christmas. However, even before then the phenomenon was of interest because of its effects on biological productivity, with its effects on the guano industry.

Normal conditions along the west Peruvian coast are a cold southerly current (the Humboldt Current) with upwelling water; the upwelling nutrients lead to great oceanic productivity; the cold currents leads to very dry conditions on land. Similar conditions exist elsewhere (California Current; Benguela Current off South Africa; West Australia Current). Thus the replacement of this with warmer northerly water leads to lower biological productivity in the ocean, and more rainfall — often flooding — on land; the connection with flooding was reported in 1895 by Pezet and Eguiguren.

Towards the end of the nineteenth century there was much interest in forecasting climate anomalies (for food production) in India and Australia. Charles Todd, in 1893, suggested that droughts in India and Australia tended to occur at the same time; Norman Lockyer noted the same in 1904. In 1924 Gilbert Walker (for whom the Walker circulation is named) first coined the term "Southern Oscillation".

For most of the twentieth century, El Niño was thought of as a largely local phenomenon.

The major 1982-3 El Niño lead to an upsurge of interest from the scientific community.

The 1998 El Niño event caused an estimated 16% of the world’s reef systems to die. Since then, mass coral bleaching has become common worldwide, with all regions having suffered ‘severe bleaching’.[19]

History of the phenomenon

ENSO conditions seem to have occurred at every two to seven years for at least the past 300 years, but most of them have been weak.

Major ENSO events have occurred in the years 1790-93, 1828, 1876-78, 1891, 1925-26, 1982-83, and 1997-98.[20]

Also, there is evidence for strong El Niño events during the early Holocene.[21]

Recent El Niños have occurred in 1986-1987, 1991-1992, 1993, 1994, 1997-1998, 2002-2003, 2004-2005 and 2006-2007.

The El Niño of 1997-1998 was particularly strong[22] and brought the phenomenon to worldwide attention. The event temporarily warmed air temperature by 1.5°C, compared to the usual increase of 0.25°C associated with El Niño events.[23] The period from 1990-1994 was unusual in that El Niños have rarely occurred in such rapid succession (but were generally weak).[24] There is some debate as to whether global warming increases the intensity and/or frequency of El Niño episodes. (see also the ENSO and Global Warming section above).

Southern Oscillation

The Southern Oscillation is an oscillation in air pressure between the tropical eastern and western Pacific Ocean waters. The strength of the Southern Oscillation is measured by the Southern Oscillation Index (SOI). The SOI is a record of the monthly or seasonal fluctuations in the normalized surface air pressure difference between Tahiti and Darwin, Australia.[25]

El Niño episodes, which are associated with negative values of the SOI, are usually accompanied by sustained warming of the central and eastern tropical Pacific Ocean, a decrease in the strength of the Pacific trade winds, and a reduction in rainfall over eastern and northern Australia. Conversely, La Niña episodes are associated with positive values of the SOI and are accompanied by stronger Pacific trade winds and warmer sea temperatures to the north of Australia. Waters in the central and eastern tropical Pacific Ocean become cooler during this time.

  • Average equatorial Pacific temperatures.
    Average equatorial Pacific temperatures.
  • El Niño effects upon North American weather and atmospheric circulation.
    El Niño effects upon North American weather and atmospheric circulation.
  • Map showing Nino3.4 and other index regions
    Map showing Nino3.4 and other index regions

See also

References

  1. ^ "El Niño Information". California Department of Fish and Game, Marine Region.
  2. ^ Pastor, Rene (2006-09-14). "El Niño climate pattern forms in Pacific Ocean". USA Today. {{cite news}}: Cite has empty unknown parameter: |coauthors= (help)
  3. ^ Borenstein, Seth (2007-02-28). "There Goes El Nino, Here Comes La Nina". CBS News. {{cite news}}: Cite has empty unknown parameter: |coauthors= (help)
  4. ^ Zebiak, S.E (1987). "A Model El Niño–Southern Oscillation". Monthly Weather Review. 115 (10): 2262–2278. doi:10.1175/1520-0493(1987)115<2262:AMENO>2.0.CO;2. Retrieved 2008-11-19. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  5. ^ Pidwirny, Michael (2006-02-02). "Chapter 7: Introduction to the Atmosphere". Fundamentals of Physical Geography. physicalgeography.net. Retrieved 2006-12-30. {{cite web}}: Check date values in: |date= (help)
  6. ^ "Envisat watches for La Nina". BNSC. 2006-03-03. Retrieved 2007-07-26.
  7. ^ "The Tropical Atmosphere Ocean Array: Gathering Data to Predict El Niño". Celebrating 200 Years. NOAA. 2007-01-08. Retrieved 2007-07-26.
  8. ^ "Ocean Surface Topography". Oceanography 101. JPL. 2006-07-05. Retrieved 2007-07-26."Annual Sea Level Data Summary Report July 2005 - June 2006" (PDF). The Australian Baseline Sea Level Monitoring Project. Bureau of Meteorology. Retrieved 2007-07-26.
  9. ^ Pearcy, W. G. (1987). "Changes in the marine biota coincident with the 1982-1983 El Niño in the northeastern subarctic Pacific Ocean". Journal of Geophysical Research. 92 (C13): 14417–14428. doi:10.1029/JC092iC13p14417. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  10. ^ Grove, Richard H. (1998). "Global Impact of the 1789–93 El Niño". Nature. 393 (6683): 318–319. doi:10.1038/30636. {{cite journal}}: Cite has empty unknown parameters: |month= and |coauthors= (help)
  11. ^ "ENSO Diagnostic Discussion". Climate Prediction Center. 2008-06-05.
  12. ^ Hong, Lynda (2008-03-13). "Recent heavy rain not caused by global warming". Channel NewsAsia. Retrieved 2008-06-22. {{cite news}}: Cite has empty unknown parameter: |coauthors= (help)
  13. ^ "9.3.5.2 Interannual variability ENSO". Climate change 2001. Intergovernmental Panel on Climate Change. 2001. Retrieved 2006-12-30.
  14. ^ Collins, Matthew (2005). "El Niño- or La Niña-like climate change?". Climate Dynamics. 24 (1): 89–104. doi:10.1007/s00382-004-0478-x. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  15. ^ Merryfield, William J. (2006). "Changes to ENSO under CO2 Doubling in a Multimodel Ensemble" (PDF). Journal of Climate. 19 (16): 4009–4027. doi:10.1175/JCLI3834.1. {{cite journal}}: Cite has empty unknown parameters: |month= and |coauthors= (help)
  16. ^ Eisenman, Ian (2005). "Westerly Wind Bursts: ENSO's Tail Rather than the Dog?". Journal of Climate. 18 (24): 5224–5238. doi:10.1175/JCLI3588.1. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  17. ^ Adams, J. Brad (2003). "Proxy evidence for an El Niño-like response to volcanic forcing". Nature. 426 (6964): 274–278. doi:10.1038/nature02101. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  18. ^ http://www.news.com.au/story/0,23599,21542564-421,00.html
  19. ^ Marshall, Paul (2006). A reef manager’s guide to coral bleaching (PDF). Townsville, Qld.: Great Barrier Reef Marine Park Authority. ISBN 1876945400. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  20. ^ Davis, Mike (2001). Late Victorian Holocausts: El Niño Famines and the Making of the Third World. London: Verso. p. 271. ISBN 1859847390.
  21. ^ Carrè, Matthieu (2005). "Strong El Niño events during the early Holocene: stable isotope evidence from Peruvian sea shells". The Holocene. 15 (1): 42–47. doi:10.1191/0959683605h1782rp. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  22. ^ Mason, S. J. (1999). "The IRI Seasonal Climate Prediction System and the 1997/98 El Niño Event" (PDF). Bulletin of the American Meteorological Society. 80: 1853–1873. doi:10.1175/1520-0477(1999)080<1853:TISCPS>2.0.CO;2. Retrieved 2008-12-15. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  23. ^ Trenberth, K. E. (2002). "Evolution of El Niño – Southern Oscillation and global atmospheric surface temperatures". Journal of Geophysical Research. 107 (D8): 4065. doi:10.1029/2000JD000298. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  24. ^ Trenberth, Kevin E. (1996). "The 1990-1995 El Niño-Southern Oscillation Event: Longest on Record". Geophysical Research Letters. 23 (1): 57–60. doi:10.1029/95GL03602. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  25. ^ Australian Bureau of Meteorology

Data sources

Further reading

Wikimedia Commons has media related to ENSO.

Template:Link FA

Retrieved from "https://en.wikipedia.org/w/index.php?title=El_Niño&oldid=281129102"