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The new face of El Niño

Date:
July 24, 2012
Source:
Institut de Recherche pour le Développement (IRD)
Summary:
Emerging once every two to seven years in the equatorial Pacific, El Niño causes disorder across the globe and for the global economy. But in the past ten years, it has changed its face. It is increasingly taking the form of Modoki, ‘similar but different’ as it was baptised by the Japanese team who first discovered this less tumultuous cousin that provokes droughts in India and Australia.

El Niño Modoki phenomena takes place above the equatorial Pacific
Credit: © IRD / B. Osès

Emerging once every two to seven years in the equatorial Pacific, El Niño causes disorder across the globe and for the global economy. But in the past ten years, it has changed its face. It is increasingly taking the form of Modoki, 'similar but different' as it was baptised by the Japanese team who first discovered this less tumultuous cousin that provokes droughts in India and Australia. Recent research has described the physical manifestations of this El Niño variant, which is centred in the central pacific, unlike its eastern relative. The impact on marine biology and its probable effects on fishing still need to be examined. To achieve this, IRD researchers and their partners from the Legos(1) and Locean(3) laboratories have studied its effects on the very first links in the food chain.

Less aquatic life in the centre of the Pacific

In the same manner as its physical mechanisms, from a biological point of view, Modoki episodes are also characterised by displacement of phenomenal effects. There is not the same widespread decrease in phytoplankton that is seen in the eastern Pacific during classic El Niño events, rather a more localised version in the central zone of the basin.

Oceanographers have observed the colouring of the Pacific using 'water colouration' satellite images taken between 1997 and 2010. The blue or green colour of the ocean seen from space actually reflects variations in the surface levels of chlorophyll. Scientists have thus observed low levels of chlorophyll in the centre of the Pacific basin (under 0.1mg per m3) during Modoki events that took place between 2002-3, 2004-5, 2006-7 and 2009-10. The concentration is an indicator of the biomass of phytoplankton at the ocean surface. In this way, the levels recorded in the central area of the basin during recent El Niño Modoki events convey the scarcity of aquatic nutrients necessary for plant development and thus for marine life forms.

When El Niño fools with the weather

Under 'normal' conditions above the Pacific, the trade winds blow strongly from east to west. They accumulate, thus confining the vast warm waters with little surface activity known as the 'warm pool' to the western part of the ocean. This enormous warm water reservoir with a temperature of over 28°C feeds the flows of warmth and humidity that affect the vast majority of the Earth's atmosphere, rather like a planetary heat pump. When a classic El Niño episode occurs, the trade winds experience a brutal drop in force, and the upwelling(4) phenomenon that is triggered all around the equator by the Coriolis effect slows down. The huge reservoir spreads out into the Pacific towards the east and the water becomes depleted.

But when Modoki occurs, the trade winds hardly drop in force. The result is a minimal slowing down of equatorial upwelling and a blockage of water from the 'warm pool' in the central basin, which in turn explains the depletion being localised in the centre of the ocean.

Colder, richer waters to the east

Another recent study, carried out in partnership with researchers from Peru(2), has recently demonstrated that Modoki type events might encourage the upwelling phenomenon which occurs in this case along the South-American coastline.

As part of their research, the team examined the surface temperature of the ocean, again observed from space and simulated using a high-resolution oceanic model. To achieve this, researchers analysed satellite images from all across Peru since 1981, and a high-resolution simulation stretching back to 1958. They thus demonstrated a cooling of the sea nearer the Peruvian coastline, corresponding to an increase in upwelling, linked to an increase in the frequency of Modoki events. This cold water rising from the deep is rich in the nutrients that support new life in the region's seas. The new face of El Niño could thus have an effect on halieutic resources around the coasts of South America.

Initially viewed by scientists as a new phenomenon, Modoki has since been proved by research to be a variant of El Niño. Indeed, Modoki is not a recent phenomenon. Researchers have found evidence of it in climate records dating back 120 years(6). However, even though a link to climate change has not yet been firmly established, its frequency may increase five times by 2050(6). Classic major episodes of El Niño from 1982-3 and 1997-8 led to a drop in fish stocks, particularly in Peru. What will happen with Modoki? The extent to which it will influence fishing resources is still to be determined.

Notes :

(1) Laboratoire d'études en géophysique et océanographie spatiales (UMR IRD / CNES / CNRS / UPS Toulouse 3)

(2) from the Discoh LMI (Imarpe, IGP and Senamhi)

(3) Laboratoire d'océanographie et du climat: expérimentations et approches numériques (UMR IRD / CNRS / MNHN / UPMC Paris 6)

(4) An 'upwelling' is a zone of cold and nutrient-rich water rising to the surface. Around the equator as a result of the Coriolis effect, masses of water moved by the trade winds are pushed towards the poles and replaced by deeper water.

(5) Instituto del Mar del Perú

(6) Nature, 2009, 461 (7263), p. 511-514. fdi:010048207


Story Source:

The above story is based on materials provided by Institut de Recherche pour le Développement (IRD). Note: Materials may be edited for content and length.


Journal References:

  1. Marie-Hélène Radenac, Fabien Léger, Awnesh Singh, Thierry Delcroix. Sea surface chlorophyll signature in the tropical Pacific during eastern and central Pacific ENSO events. Journal of Geophysical Research, 2012; 117 (C4) DOI: 10.1029/2011JC007841
  2. B. Dewitte, J. Vazquez-Cuervo, K. Goubanova, S. Illig, K. Takahashi, G. Cambon, S. Purca, D. Correa, D. Gutierrez, A. Sifeddine, L. Ortlieb. Change in El Niño flavours over 1958–2008: Implications for the long-term trend of the upwelling off Peru. Deep Sea Research Part II: Topical Studies in Oceanography, 2012; DOI: 10.1016/j.dsr2.2012.04.011

Cite This Page:

Institut de Recherche pour le Développement (IRD). "The new face of El Niño." ScienceDaily. ScienceDaily, 24 July 2012. <www.sciencedaily.com/releases/2012/07/120724104302.htm>.
Institut de Recherche pour le Développement (IRD). (2012, July 24). The new face of El Niño. ScienceDaily. Retrieved September 2, 2014 from www.sciencedaily.com/releases/2012/07/120724104302.htm
Institut de Recherche pour le Développement (IRD). "The new face of El Niño." ScienceDaily. www.sciencedaily.com/releases/2012/07/120724104302.htm (accessed September 2, 2014).

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