Natural Climate Variability — Explain natural climate variability (ENSO) conceptually

For centuries, fishermen along the western coast of South America noticed something strange. Every few years, the normally cool, fish-rich waters off Peru and Ecuador would turn unusually warm around Christmastime. The fish would vanish, and heavy rains would pound areas that were usually dry. Local fishermen called this mysterious warming El Niño, meaning "The Little Boy" or "The Christ Child," because it often arrived near Christmas. What they didn't yet realize was that this local event was part of a massive, planet-spanning climate pattern.

Scientists spent decades piecing together the puzzle. They discovered that the warming off South America was connected to changes in wind patterns, ocean currents, and air pressure stretching across the entire Pacific Ocean. This phenomenon — now called ENSO (El Niño–Southern Oscillation) — is one of the most powerful examples of natural climate variability on Earth.

The central question ENSO raises is this: How can a shift in ocean temperature in one part of the world change weather patterns across the entire globe? Understanding ENSO helps us see that Earth's climate is not static — it naturally oscillates, and those oscillations have real consequences for people everywhere.

Before diving into how ENSO works, let's establish some key ideas. ENSO is not a single event — it is a cycle with three phases that repeat every two to seven years. Understanding the vocabulary and the core principles behind this cycle will help everything else make sense.

The diagram below shows the tropical Pacific Ocean during the three ENSO phases. Pay close attention to how the trade winds, the warm water pool, and the thermocline (the boundary between warm surface water and cold deep water) shift in each phase.

During neutral conditions, the trade winds blow steadily from east to west. They push warm surface water toward Australia and Indonesia, where it piles up. The thermocline tilts — it is deep in the west and shallow in the east. This shallow thermocline in the east allows cold, nutrient-rich water to well up to the surface, keeping the eastern Pacific cool and supporting rich fisheries.

During El Niño, the trade winds weaken or even reverse direction. Without strong winds pushing water westward, the warm pool spreads eastward across the Pacific. The thermocline flattens out, cutting off the cold upwelling in the east. Sea surface temperatures in the central and eastern Pacific rise significantly — often by 1.5°C to 3°C above normal.

During La Niña, the trade winds blow even harder than normal. They push the warm pool tightly against the western Pacific coast and pull the thermocline especially close to the surface in the east. Cold upwelling intensifies, making the eastern Pacific cooler than average. La Niña is essentially a supercharged version of the normal pattern.

What makes ENSO so powerful is a positive feedback loop between the ocean and the atmosphere. In a positive feedback loop, a small change in one part of the system causes a change in another part, which then amplifies the original change. This is sometimes called the Bjerknes feedback, named after the scientist who first described it.

The Bjerknes Feedback — Step by Step

Imagine the trade winds weaken slightly due to random weather fluctuations. Here is what happens next. Warm water, which was being pushed westward, begins to spread eastward. The warmer eastern Pacific heats the air above it. Hot air rises, creating a zone of low pressure over the central Pacific. This low-pressure zone further weakens the trade winds because winds blow from high pressure to low pressure — and the pressure difference that drives the trade winds decreases. With even weaker trade winds, even more warm water slides east. The cycle reinforces itself.

You might wonder: if the feedback loop keeps amplifying, why doesn't El Niño just keep getting stronger forever? The answer is that negative feedbacks eventually kick in. As warm water spreads east, it exposes cooler water in the western Pacific. This changes air circulation patterns and eventually allows the trade winds to strengthen again. Oceanic waves called Kelvin waves and Rossby waves travel across the Pacific and help "reset" the system, often swinging conditions toward La Niña.

ENSO doesn't just affect the Pacific Ocean — its influence reaches across the globe through teleconnections. When the pattern of rising and sinking air shifts over the Pacific, it sends ripples through the atmosphere that alter jet stream positions, storm tracks, and rainfall patterns in distant regions. The table below compares the typical impacts of El Niño and La Niña on different parts of the world.

One of the most striking impacts of El Niño is its effect on global average temperature. During a strong El Niño, the release of heat from the Pacific Ocean into the atmosphere can temporarily raise global temperatures by about 0.1–0.2°C. This is why some of the warmest years on record — such as 1998, 2016, and 2023 — coincided with strong El Niño events. However, this warming is temporary. La Niña years tend to be slightly cooler than average.

Scientists use a measurement called the Oceanic Niño Index (ONI) to officially classify ENSO phases. The ONI measures how much the sea surface temperature in the Niño 3.4 region departs from its long-term average. If the ONI stays above +0.5°C for at least five consecutive overlapping three-month periods, it is classified as El Niño. If it stays below −0.5°C for the same duration, it is La Niña. Values between −0.5°C and +0.5°C indicate neutral conditions.

El Niño and La Niña are opposite phases of the same cycle, but they are not simply mirror images. Their impacts differ in intensity and distribution. The following table provides a side-by-side comparison of the most important features of each phase.

A common question is: if ENSO causes natural warming and cooling, does that mean current global warming is just part of a natural cycle? The answer is no. ENSO and human-caused (anthropogenic) climate change are fundamentally different phenomena. Understanding how they relate to each other is important for thinking clearly about Earth's climate.

Think of it this way: climate change is like slowly raising the water level in a swimming pool, while ENSO is like the waves sloshing back and forth. The waves (ENSO) create natural ups and downs, but the overall water level (long-term temperature trend) keeps rising due to greenhouse gas emissions. This means that El Niño events today start from a warmer baseline than they did 50 years ago, making record-breaking temperatures more likely.