Who's in Charge in the Ocean–Atmosphere Duo? ✎

Original: "Inferring directed climatic interactions with renormalized partial directed coherence and directed partial correlation"
arXiv:1706.06096 · 2017-06-19 · arXiv non-exclusive · independent analysis · 1 min
Scientists have found a way to hear how the ocean and atmosphere influence each other, even when the signals are weak and noisy.

A translator who hears only the meaning, not the noise in the hall, can accurately convey a conversation. Climatologists need such a translator to understand how the ocean and atmosphere influence each other. Their interaction resembles a conversation where voices are drowned out by background sounds. In a new study, tools originally designed for analyzing brain signals have been applied to climate data for the first time.

The brain and climate are similar: important connections are weak, while noise is strong.

The methods work like an attentive listener. They don't just see that two signals change together; they compute which one sounds first. To do this, they build a model where the current value depends on the past of both signals, and noise is accounted for separately. The methods were first tested on synthetic data where the direction of influence is known. There, they clearly identified the correct direction, while the old method made mistakes.

Next, they took real data: ocean temperature in the tropical Pacific and rainfall over India. All methods agreed: El Niño influences the monsoon more strongly than the monsoon influences El Niño, and the connection lags by one to two years. For the South Atlantic Convergence Zone, the new method revealed, for the first time, years when the ocean truly drives the atmosphere. Now climatologists can test such connections in other regions, for example, how the ocean affects droughts.

The NINO3.4 index used in the study is calculated from sea surface temperatures over an area roughly the size of Australia. The average temperature anomaly there changes by only a few tenths of a degree, yet that is enough to alter weather on the other side of the planet.

Concepts
seasonal forcing NOAA CPC granger causality coupled general circulation model North Equatorial Countercurrent Teleconnection ENSO ocean-atmosphere coupling climate network intertropical convergence zone PCR ocean current reanalysis direct current linear regression cross correlation Multivariate ENSO Index