Corpus ID: 116007213

Sloshing Model for ENSO

@article{Pukite2014SloshingMF,
  title={Sloshing Model for ENSO},
  author={P. Pukite},
  journal={arXiv: Atmospheric and Oceanic Physics},
  year={2014}
}

P. Pukite

Published 2014

Physics

arXiv: Atmospheric and Oceanic Physics

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The El Nino southern oscillation (ENSO) behavior can be effectively modeled as a response to a 2nd-order Mathieu/Hill differential equation with periodic coefficients describing sloshing of a volume of water. The forcing of the equation derives from QBO, angular momentum changes synchronized with the Chandler wobble, and solar insolation variations. One regime change was identified in 1980.