El Niño Southern Oscillation

What is El Niño - Southern Oscillation?

What is El Niño? 

The El Niño Southern Oscillation (ENSO) is a large-scale climatic phenomenon that originates in the tropical Pacific but affects global climate patterns. The warm phase is known as El Niño and the cold phase is La Niña. El Niño occurs irregularly every two to seven years and peaks around in winter. 

What causes an El Niño event?

In a normal year, when ENSO is inactive, the equatorial Pacific trade winds blow from east to west. The winds push the warmer water towards the west, and colder water rises up from deeper in the ocean to replace it. This creates an east-west difference in sea surface temperature and hence an east-west difference in sea level pressure that maintains the trade winds and so drives a positive feedback loop. 

During an El Niño year, the east-west SST difference weakens, the pressure difference weakens and the trade winds and their effects on the ocean weaken, so the eastern Pacific warms further. During a La Niña year, the opposite happens, the east west difference in temperature strengthens, the pressure difference strengthens and the trade winds and their effects on the ocean strengthen, so the east Pacific cools further.

Such changes in sea surface temperatures affect the atmosphere over vast areas, with both local and global repercussions. Locally, the associated atmospheric circulation changes drive increased atmospheric convection and precipitation over the central and eastern Pacific while rainfall is reduced over the western Pacific. These changes have remote impacts throughout the tropics but also at higher latitudes via the atmosphere, especially when ENSO is at its strongest in winter.

How do we measure El Niño? 

A network of ocean buoys measure water temperature, currents and the wind. Satellites also provide surface temperature and current data, providing the ability to monitor ENSO in real-time. We are also able to predict El Niño months in advance as we can measure the heat content of the upper-ocean, one of the precursors for the onset of El Niño and use our climate models to predict its evolution. Although various criteria exist, we normally say an El Niño event is underway when sea surface temperatures in the equatorial Pacific (officially called Niño region 3.4), rise 0.5°C above the historical average for at least three months in a row. 

Impacts of El Niño and La Niña

The strongest impacts are experienced by those countries near the tropical Pacific origin of ENSO. Changes in surface temperatures, winds and moisture affect rainfall intensity and patterns which can lead to extreme events such as flooding and drought. During an El Niño event, Peru, Ecuador and south-eastern parts of South America receive heavy rainfall. In northern Brazil, drier conditions or even drought results. Indonesia, South Asia and parts of Australia are also more likely to experience drought during El Niño. The change in weather patterns associated with El Niño can greatly impact the economy, in particular agriculture, water resources, fisheries and public health. ENSO also has a strong influence on the occurrence and intensity of tropical cyclones and Atlantic hurricane activity weakens during El Niño but strengthens during La Niña. In the UK, we experience the socio-economic impacts of an El Niño event, partly through increased food prices and there are effects on the jet stream and European weather, especially in late winter when El Niño increases the chances of cold snaps and La Niña increases the chances of wet and stormy conditions.

How does El Niño affect global temperature?

El Niño releases heat to the atmosphere and increases subsequent global temperatures. For example, global average temperatures for 2016 were around 1.1°C above preindustrial values and the strong El Niño episode of 2015/2016 partly contributed. However, researchers have concluded that the warming from El Niño is only accountable for about 0.2°C of this overall figure. 

El Niño and climate change

Because of the large event to event variations of El Niño, we don’t have enough past years of observations to show a clear impact of climate change on its properties. There is now some evidence that the effects of El Niño on rainfall may increase in the future and that we may even see more very strong ENSO events, but these remain active research questions. 

Schematic of the El Niño Southern Oscillation
Figure redrawn from NOAA 


Listen to the Society's podcast about El Niño and La Niña with Professor Adam Scaife.

Categories: Climate
Tags: Atmospheric Dynamics Climate Ocean Teleconnections WorldWeather

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