El Niño Without a Teacher: How an Algorithm Heard Climate in Ocean Noise ✎

Original: "Unsupervised Discovery of El Nino Using Causal Feature Learning on Microlevel Climate Data"
arXiv:1605.09370 · 2016-05-30 · arXiv non-exclusive · independent analysis · 2 min
An algorithm independently picked out El Niño and La Niña from raw wind and ocean temperature data.

A translator sits in a hall where people speak an unfamiliar language. They don't understand the words, but they hear how the tone shifts: sometimes calm and steady, sometimes excited and sharp. From intonation alone, they guess what is being discussed. That is roughly what an algorithm did when given thirty-six years of observations from the equatorial Pacific: week by week, wind and water temperature. No one told it what El Niño is. It heard two states familiar to climatologists in that data on its own.

El Niño is the warm phase of a climate oscillation in the Pacific Ocean, while La Niña is the cold phase of the same oscillation.

Previously, climatologists identified El Niño manually: they took surface temperatures at specific points in the ocean and checked how far they deviated from the average. If the deviation exceeded a threshold, they declared an event. That method is simple, but it relies on pre-selected points and thresholds. What if the phenomenon manifests differently than expected? The algorithm from the new study works differently: it first learns to predict temperature from wind, then looks for which stable combinations of wind and temperature occur most often. Those combinations become the climate's "intonations."

Zonal wind is wind that blows along a parallel from west to east. In this region of the ocean, it is closely linked to water temperature.

The result was four wind states and four temperature states. Two of them matched El Niño and La Niña almost exactly: in these states, weeks with a warm anomaly above 0.5 degrees occurred three times more often than in the others. For comparison, ordinary data clustering into 16 groups did not achieve such accuracy. And when the data were shuffled randomly, the algorithm found nothing significant at all. This means it captured a real causal link between wind and water, not random coincidences.

The translator did not learn the language, but they learned to tell when the speaker is calm and when alarmed. Likewise, the algorithm does not know ocean physics, but it has learned to identify states that climatologists call El Niño and La Niña. This approach can now be applied to other pairs of measurements, such as pressure and precipitation. Perhaps we will be able to hear new "intonations" in the climate that we have not noticed so far.

The name 'El Niño' comes from the Spanish for 'the Christ child,' because the warm current often appears around Christmas.

Concepts
El Niño La Niña ENSO ERSST zebiak cane model El Niño index Westerly wind burst NOAA CPC Multivariate ENSO Index relative ONI Jin-Timmermann model natural variability spring predictability barrier NOAA PMEL / TAO seasonal cycle Bjerknes feedback Indian Ocean capacitor effect Southern Oscillation equatorial wave propagation TAO/TRITON moorings