Why a Warm Current Doesn't Always Weaken Monsoon Rains ✎

Original: "Reconsidering the relationship of the El Niño--Southern Oscillation and the Indian monsoon using ensembles in Earth system models"
arXiv:1803.08909 · 2018-03-23 · arXiv non-exclusive · independent analysis · 1 min
Scientists ran a hundred identical climate models to understand how a warm Pacific current relates to rains over India.

Sometimes the ocean and the sky dance together. When the warm current El Niño arrives in the Pacific, rains over India usually quiet down. But in recent decades, this dance has stumbled: rains don't always follow the warm water. Scientists set out to find out why.

Earlier, they simply looked at average values over many years. That's like trying to understand a dance from a single photograph. Now they've been smarter: they ran a hundred identical climate models with slightly different starting conditions. After forty years, all these models, like dancers, find a common rhythm. From their spread, you can precisely measure the connection.

A hundred models instead of one help separate random fluctuations from real changes.

It turned out that over the past century, the link between the warm current and rains became stronger. But when the models looked into the future, where greenhouse gas emissions rise, the link didn't change. The dance stayed the same, even though the music got louder. So, it's not just about warming. Now scientists want to test this method on other pairs, for example, the link between El Niño and rains in Africa.

The sea-level pressure difference between Tahiti and Darwin used in this study underlies the Southern Oscillation, an index that meteorologists have been calculating for over a century.

r = \frac{\langle p_{diff} P \rangle - \langle p_{diff} \rangle \langle P \rangle}{\sqrt{(\langle p_{diff}^2 \rangle - \langle p_{diff} \rangle^2)(\langle P^2 \rangle - \langle P \rangle^2)}}
Angle brackets denote ensemble averaging, not time averaging
Concepts
Multivariate ENSO Index ENSO El Niño-Southern Oscillation Jin-Timmermann model Southern Oscillation spring predictability barrier El Niño index Teleconnection recharge oscillator model TAO/TRITON moorings interannual variability monsoon monsoon onset La Niña ocean-atmosphere coupling ERSST Indian Ocean capacitor effect natural variability relative ONI ensemble forecast