# Three-dimensional slow Rossby waves in rotating spherical density stratified convection

## TL;DR

This paper develops a theory of three-dimensional slow Rossby waves in rotating spherical density stratified convection, linking them to planetary phenomena like El Niño and the Southern Oscillation, with predictions matching observations.

## Contribution

The paper introduces a new theoretical framework for slow Rossby waves in stratified convection, explaining their connection to long-term climate oscillations.

## Key findings

- Theoretical predictions align with observed SOI periods.
- Identifies Rossby waves as a mechanism behind El Niño and Southern Oscillation.
- Provides a new interpretation of planetary climate variability.

## Abstract

We develop a theory of three-dimensional slow Rossby waves in rotating spherical density stratified convection. The Rossby waves with frequencies which are much smaller than the rotating frequency, are excited by a non-axisymmetric instability from the equilibrium based on the developed convection. These waves interact with the inertial waves and the density stratified convection. The density stratification is taken into account using the anelastic approximation for very low-Mach-number flows. We study long-term planetary Rossby waves with periods which are larger than two years. We suggest that these waves are related to the Southern Oscillation and El Ni\~{n}o. The El Ni\~{n}o is an irregularly periodical variation in winds and sea surface temperatures over the tropical Pacific Ocean, while the Southern Oscillation is an oscillation in surface air pressure between the tropical eastern and the western Pacific Ocean. The strength of the Southern Oscillation is characterised by the Southern Oscillation Index (SOI). The developed theory is applied for the interpretation of the observed periods of the SOI. This study demonstrates a good agreement between the theoretical predictions and the observations.