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Global temperatures have been rising steadily due to climate change, but the onset of the 2023 El Niño cycle has supercharged this warming trend, pushing global temperatures to unprecedented levels. As El Niño took hold, 2023 became one of the hottest years on record, and its ripple effects have triggered extreme weather events worldwide. However, with El Niño now officially ending, the world is preparing for a potential transition to La Niña, which could bring a new set of climate impacts.
👉 In this article, we'll explore what El Niño is, how it interacts with climate change, and the potential global consequences.
El Niño was first observed by South American fishermen, who noticed a periodic warming of the ocean waters around Christmas time. They named it El Niño de Navidad - meaning "the Christ Child" - because it often peaks around December. Though initially known only in the Pacific region, scientists have since discovered that El Niño’s influence extends well beyond, affecting global weather patterns.
Its impacts range from intense droughts in some areas to increased rainfall and flooding in others. The most recent El Niño, which began in 2023, played a major role in fueling record-high global temperatures and extreme weather worldwide. Although El Niño is now coming to an end, its aftereffects will continue to shape global weather, and the world is now preparing for a likely transition to La Niña.
El Niño means "the Little Boy" or "the Christ Child" in Spanish, it is just one phase of a broader climate phenomenon known as the El Niño Southern Oscillation (ENSO), which sees the Earth’s climate system oscillate between two opposite extremes: El Niño and La Niña. La Niña, meaning "the Little Girl," represents the cooler counterpart to El Niño. This cycle typically spans 3 to 7 years, with 5 years being the average. The ENSO cycle plays a key role in shaping weather patterns across the globe, leading to fluctuations between warm (El Niño) and cool (La Niña) oceanic conditions in the Pacific.
La Niña is the counterpart to El Niño and represents a period of unusually cool sea surface temperatures in the equatorial Pacific. During La Niña events, temperatures can drop 3 to 5 degrees Celsius below the average, often resulting in cooler, drier weather in the tropical eastern Pacific region. However, much like El Niño, La Niña’s impacts are far-reaching, with global consequences such as increased rainfall in some regions and drought in others.
The cycle’s timing is also critical. El Niño and La Niña events generally form between March and June but reach their peak between December and April, when their effects on global weather are most pronounced. El Niño typically lasts 9 to 12 months, although some episodes can extend for 3 to 4 years, as seen in recent decades. La Niña, on the other hand, tends to last longer, usually persisting for 1 to 3 years.
👉 It’s also important to note that in some years, neutral conditions prevail, where sea surface temperatures in the Pacific are closer to the long-term average. In fact, about half of all years fall into this "neutral" category, where neither El Niño nor La Niña dominates the climate system.
While the warming effects of El Niño are often mistakenly linked to climate change, the El Niño Southern Oscillation (ENSO) is actually a natural climate cycle that has been influencing global weather patterns for thousands of years. ENSO represents a periodic fluctuation in sea surface temperatures and atmospheric pressure across the equatorial Pacific, driving changes in global weather systems. This oscillation between warm (El Niño), cool (La Niña), and neutral phases affects tropical rainfall, wind patterns, and ocean currents, with significant impacts on climate worldwide.
Under normal (neutral) conditions, the tropical Pacific Ocean is characterised by stable trade winds that blow from east to west along the equator. These trade winds push the sun-warmed surface waters from the cooler eastern Pacific (near South America) toward the western Pacific Ocean (near Indonesia and Australia). As a result, sea surface temperatures in the western Pacific become significantly warmer - by 8 to 10 degrees Celsius - compared to the eastern Pacific.
This temperature difference drives atmospheric circulation. The warmer waters in the west generate low-pressure zones and create hot, humid conditions, leading to frequent rainfall in the western Pacific. Meanwhile, the cooler waters in the eastern Pacific maintain higher air pressure, creating drier and cooler weather along the western coast of South America. This balance of wind and ocean currents is the neutral state of the ENSO cycle.
During an El Niño event, this equilibrium is disrupted. The trade winds, which normally push warm water westward, weaken or even reverse, blowing in an easterly direction. This allows the warm water that is typically confined to the western Pacific to spread eastward toward the central and eastern parts of the ocean. As a result, sea surface temperatures in the eastern Pacific rise dramatically, and the usual temperature contrast between the east and west Pacific is diminished.
The intensity of El Niño events can vary significantly. In weaker El Niño episodes, sea surface temperature increases may be relatively modest, around 2–3°C, leading to only moderate local effects on weather patterns. However, during stronger events, sea surface temperatures can increase by as much as 8–10°C, triggering far-reaching and often severe climatic changes across the globe.
This shift in ocean temperatures triggers a chain reaction in the atmosphere. Higher air pressure builds over the western Pacific (around the Indian Ocean, Indonesia, and Australia), while lower pressure develops over the central and eastern tropical Pacific Ocean. The reversal of these pressure patterns leads to changes in tropical rainfall: drier-than-usual conditions and droughts impact the western Pacific, while wetter, stormier weather affects the eastern Pacific, including the coasts of South America and North America. These altered circulation patterns can result in flooding in some regions and droughts in others, with the intensity of these impacts closely linked to the strength of the El Niño event.
In contrast, La Niña represents the cooling phase of the ENSO cycle and occurs when the trade winds intensify rather than weaken. These stronger winds push the warm surface waters of the western Pacific even further west, allowing colder, nutrient-rich deep ocean water to upwell along the equatorial eastern Pacific, particularly near the western coast of South America. This phenomenon causes the sea surface temperatures in the eastern Pacific to drop by 3 to 5 degrees Celsius below average.
As the ocean cools, atmospheric patterns shift again. Low pressure dominates the western Pacific, bringing wetter conditions to regions like Southeast Asia and northern Australia. Meanwhile, high pressure strengthens in the eastern Pacific, contributing to drier and cooler weather in South America. The intensified trade winds and cooler ocean temperatures also reduce the likelihood of tropical storm activity in the eastern Pacific while increasing storm activity in other parts of the world, such as the Atlantic basin.
Although El Niño and La Niña primarily originate in the Pacific Ocean, their reach extends across the globe. El Niño is often linked to increased storm activity and warmer global temperatures, while La Niña tends to cool the planet slightly and enhance the likelihood of hurricanes in the Atlantic. Both phases of ENSO cause dramatic shifts in rainfall, drought patterns, and storm intensities, influencing weather across continents and affecting ecosystems, agriculture, and economies around the world.
El Niño and La Niña are powerful climate phenomena that significantly alter global weather patterns, but their impacts vary greatly depending on geographic location, the intensity of the event, the time of year, and other interacting climate systems. No two El Niño or La Niña events are the same, making them challenging to study and predict. Understanding these phenomena is essential for anticipating extreme weather events and preparing for their impacts.
During an El Niño event, the weakening of trade winds allows warm water to move eastward toward the coast of the Americas. This shift causes an array of weather disruptions across the globe:
La Niña, the colder counterpart to El Niño, typically reverses these effects by enhancing trade winds and pushing warm water further west:
| Region | Impact During El Niño | Impact During La Niña |
|---|---|---|
| North America | Wetter southern U.S.; reduced hurricane activity in the Atlantic | Colder, stormier winters in the northern U.S.; drier in the south |
| South America (North) | Drier in northern regions, reduced rainfall | Increased rainfall in northern Brazil |
| South America (South) | Wetter conditions, increased flooding in southern regions | Drier-than-normal conditions, particularly in southern regions |
| Africa (Horn of Africa) | Increased rainfall, potential for flooding | Drier conditions |
| Africa (Southern) | Drier conditions, drought, and increased wildfire risk | Wetter conditions, flooding in southeastern Africa |
| Australia | Drier conditions, risk of drought and wildfires | Wetter conditions, increased flooding |
| Southeast Asia | Drier, warmer conditions, increased risk of wildfires | Wetter, cooler conditions, increased rainfall |
| East Asia (Central Asia) | Increased rainfall, potential for flooding | Drier conditions |
| Pacific Ocean | Increased hurricane activity in the central and eastern Pacific | Reduced hurricane activity in the central and eastern Pacific |
| Atlantic Ocean | Decreased hurricane activity | Increased hurricane activity |
| Europe | Warmer winters, wetter conditions (especially southern Europe) | Colder winters, potential for drier southern conditions |
Although El Niño and La Niña are natural climate phenomena that have shaped weather patterns for millennia, mounting evidence suggests that climate change is influencing their frequency, intensity, and predictability. While the El Niño Southern Oscillation (ENSO) cycle itself is not caused by climate change, the growing heat trapped in the world’s oceans may be disrupting the established relationships between these phenomena and weather patterns.
Since the 1970s, El Niño events have occurred more frequently and lasted longer, raising questions about whether rising global sea surface temperatures are facilitating the development and persistence of these events. The additional heat stored in oceans due to human-induced climate change may be altering normal ocean circulation patterns and amplifying the strength of ENSO cycles.
However, new research highlights the challenges in predicting ENSO events in the context of climate change. According to the Bureau of Meteorology (BoM) in Australia, global heating is making historical models of El Niño and La Niña less reliable. Dr. Karl Braganza, BoM’s national manager of climate services, emphasized that while the climate system hasn’t “broken,” the relationships between ENSO and regional weather patterns are becoming less consistent.
For example, in the past, El Niño was strongly associated with warmer and drier conditions in regions like Australia and Indonesia, while La Niña brought cooler and wetter weather. However, these links are becoming more unpredictable as heat builds in the oceans, making the past less useful for forecasting the future. Dynamical models that consider real-time ocean and atmospheric conditions, including greenhouse gas concentrations, are now more effective than older statistical models based on historical data.
Regardless of how climate change directly affects the ENSO cycle, it is clear that the combination of global warming and ENSO events is exacerbating extreme weather patterns. As temperatures rise globally, ENSO events appear to trigger more severe climatic responses, including intensified storms, droughts, and temperature extremes.
Dr. Braganza noted that forecasts for ENSO events must now account for these uncertainties. For example, the 2023 El Niño initially brought hot, dry conditions to Australia, but unexpectedly, torrential rains followed in December and January, highlighting the growing unpredictability of ENSO’s effects under climate change.
Global meteorological agencies are adapting their forecasting models to reflect the increasing unpredictability of El Niño and La Niña in a warming world. Dynamical models, such as BoM’s ACCESS-S, which use real-time ocean and atmosphere observations, are now more reliable than historical data alone. These models offer probabilistic forecasts, which help communities assess the likelihood of different weather outcomes, allowing them to better hedge their risks and prepare for extreme weather.
As the Earth continues to warm, the interplay between ENSO and climate change is likely to lead to even more intense and unpredictable weather patterns. The 2023-2024 El Niño event pushed global temperatures to record highs, and future El Niño and La Niña events are expected to continue exacerbating weather extremes, especially in regions vulnerable to their impacts.
While much research remains to be done, one thing is certain: the impacts of ENSO will grow more severe in a warming world, making it crucial for governments, businesses, and communities to improve climate resilience and rely on long-range forecasts based on current climate data rather than outdated historical trends.
The 2023-2024 El Niño cycle, which began in June 2023 and contributed to some of the hottest global temperatures on record, has now officially ended. In June 2024, both the World Meteorological Organization (WMO) and the US National Oceanic and Atmospheric Administration (NOAA) confirmed that El Niño conditions are no longer present. As the cycle ends, scientists are now predicting a possible transition to La Niña conditions, which could bring its own set of global impacts.
The El Niño event of 2023-2024 had profound effects on global weather patterns, pushing temperatures and extreme weather events to new highs:
As El Niño ends, attention is now shifting toward a possible La Niña event, which is predicted to develop later in 2024. The WMO forecasts at least a 60% chance of La Niña conditions developing by the end of 2024.
The 2023-2024 El Niño demonstrated how these natural climate phenomena, when combined with long-term global warming, can push global weather to extremes. While El Niño temporarily increased global temperatures, its end does not mean a break from the broader trend of climate change. The record-high sea surface temperatures observed during this period are likely to persist, contributing to continued warming even as the planet transitions into La Niña.
Furthermore, La Niña’s cooling effect will likely be modest, as the planet's overall warming trend continues. The impact of La Niña will be closely monitored, particularly in regions vulnerable to its effects, such as Southeast Asia and the Atlantic hurricane basin.
It is clear that while El Niño is over, the world remains on edge as La Niña takes center stage. The combined effects of these climate phenomena with global warming will continue to shape weather patterns worldwide, reinforcing the need for early warnings and preparedness.
Even though the science is not clear on whether or not climate change is impacting the El Niño Southern Oscillation cycle, what is clear is that El Niño and La Niña have the potential to exacerbate the impacts of global warming.
We’re now heading into another El Niño period, and even though the most extreme effects are not expected to be felt until 2024, the combination of climate change and El Niño means that we are entering uncharted territory.
This is why it’s so important to understand and study the El Niño Southern Oscillation cycle. It is essential for predictive modelling that can help us to anticipate and therefore mitigate or adapt to the worst effects of these cycles.
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