Why India's rains can be predicted 18 months ahead ✛ ✎

Original: "Resolving the Paradox of Changing El Niño-Monsoon Relation through Synchronization of Chaotic Oscillators"
arXiv:2603.16346 · 2026-03-17 · arXiv non-exclusive · independent analysis · 1 min
Deep ocean waters and the Indian monsoon resonate with an 18-month lag, and this link does not weaken over time.

Two pendulums hang on the same wall, swinging out of sync, but suddenly they start moving as one, only with a delay of eighteen months. One pendulum is the Indian monsoon, the seasonal wind that brings rain to the fields of South Asia. The second is the deep waters of the tropical oceans, which slowly accumulate heat and remember it for years.

Previously, scientists looked at the surface temperature of the Pacific Ocean to predict rains in India. But the connection would strengthen and weaken, and it seemed that forecasting was impossible. Then they thought to look deeper, at the water layer where the temperature reaches 20°C. This layer changes slowly and holds the ocean's memory for years, unlike the surface, which forgets everything within a few months.

It turned out that the deep ocean layer and monsoon rainfall resonate with an 18-month lag. It's like two pendulums that start swinging in sync, but one lags behind by a year and a half.

Now it is possible to make forecasts of the Indian monsoon 18 months ahead. This is important for farmers planning their sowing, and for cities stocking up on water. Two pendulums on the same wall do not just swing side by side; they hear each other through the ocean's depths.

The depth of the 20°C isotherm in the tropics changes by tens of meters, and these slow waves remember the ocean state for years, while the surface forgets everything within a few months.

PLV = \left| \frac{1}{N} \sum_{t=1}^{N} e^{i\Delta\phi(t)} \right|
A measure of how stably two oscillatory systems maintain their phase difference
Concepts
interannual variability El Niño ENSO El Niño-Southern Oscillation monsoon monsoon onset La Niña spring predictability barrier Indian Ocean capacitor effect Multivariate ENSO Index Southern Oscillation Indian Ocean Dipole relative ONI seasonal cycle natural variability seasonal forcing Jin-Timmermann model TAO/TRITON moorings recharge oscillator model ERSST