Nonlinear Recharge Oscillator
Abstract
The El Nino-Southern Oscillation (ENSO) is not a simple linear system but a non-linear system. Obviously, nonlinear properties of ENSO cannot be explained by a simple linear recharge oscillator model (linear ROM). Therefore, we develop a nonlinear ROM by adding square terms into a linear ROM. The square terms are dynamically derived from nonlinear dynamical heating. The nonlinear dynamical heating has been known as a driver of amplitude asymmetry of ENSO. Using a Fokker Plank equation, we compute a probability function of a nonlinear and linear ROMs. The probability function of nonlinear ROM clearly demonstrates a skewed probability density and a non-symmetric oscillatory behavior as seen in the observation. Finally, the linear ROM well explains amplitude and period of ENSO, while the nonlinear ROM additionally explains the skewness and non-symmetric oscillatory feature of ENSO.
- Publication:
-
AGU Fall Meeting Abstracts
- Pub Date:
- December 2018
- Bibcode:
- 2018AGUFMGC33I1466A
- Keywords:
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- 3339 Ocean/atmosphere interactions;
- ATMOSPHERIC PROCESSESDE: 1627 Coupled models of the climate system;
- GLOBAL CHANGEDE: 4522 ENSO;
- OCEANOGRAPHY: PHYSICALDE: 4922 El Nino;
- PALEOCEANOGRAPHY