How to Predict El Niño ✎

Original: "Machine learning of committor functions for predicting high impact climate events"
arXiv:1910.11736 · 2019-10-25 · arXiv non-exclusive · independent analysis · 1 min
The probability of a future event depends on where the system is now, and this dependence can be learned.

When a meteorologist talks about the chance of rain, they rely on the current state of the atmosphere: pressure, humidity, wind. Similarly, for rare climate events, such as a strong El Niño, the warm current off the coast of South America, one can build a probability map. On this map, each point corresponds to a specific state of the ocean and atmosphere, and the color shows the probability that an event will start from there.

The committor function is the probability of reaching a threshold within a given time. It varies for each starting point. Instead of a single forecast, we get an entire probability map.

But how do you build such a map? The direct way is to run many simulations from each point and count the fraction that lead to the event. That is very expensive. Instead, the scientists trained a neural network on pairs of initial state and outcome, and it learned to predict the probability. Tests on a simple model showed that the network makes only small errors.

It turns out that the map has four types of regions. In some, the probability is always 0 or 1, meaning the outcome is predetermined. In others, the probability changes smoothly, so forecasting is possible but not precise. And there are regions where the slightest change in the starting point flips the probability from 0 to 1. There, forecasting is practically impossible. Knowing where these regions are helps to honestly assess forecast uncertainty.

In the Jin-Timmermann model, the two attractors, periodic and chaotic, are intertwined in state space like threads in a tangle, so that arbitrarily close initial points can lead to completely different fates.

Concepts
Jin-Timmermann model forecast spring predictability barrier El Niño-Southern Oscillation Multivariate ENSO Index El Niño probabilistic forecast ENSO predictability prediction equatorial wave propagation La Niña NOAA CPC recharge oscillator model prediction error ERSST North Atlantic Oscillation Indian Ocean capacitor effect Warm water volume interannual variability