2007
DOI: 10.1119/1.2358155
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El Niño and the delayed action oscillator

Abstract: We study the dynamics of the El Niño phenomenon using the mathematical model of delayedaction oscillator (DAO). Topics such as the influence of the annual cycle, global warming, stochastic influences due to weather conditions and even off-equatorial heat-sinks can all be discussed using only modest analytical and numerical resources. Thus the DAO allows for a pedagogical introduction to the science of El Niño and La Niña while at the same time avoiding the need for large-scale computing resources normally asso… Show more

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Cited by 62 publications
(35 citation statements)
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“…For instance, in the cases of communication in neuronal systems [37], proper functioning in cardiac and respiratory systems [38], and specific physiological processes [39] such as cell necrosis within organs [40], stable and robust global oscillation is quite essential. Even from the perspective of power grids [41] and the El Niño or southern oscillation in Earth's ocean and atmosphere [42], the study of dynamical rhythmicity is very important.…”
Section: Discussionmentioning
confidence: 99%
“…For instance, in the cases of communication in neuronal systems [37], proper functioning in cardiac and respiratory systems [38], and specific physiological processes [39] such as cell necrosis within organs [40], stable and robust global oscillation is quite essential. Even from the perspective of power grids [41] and the El Niño or southern oscillation in Earth's ocean and atmosphere [42], the study of dynamical rhythmicity is very important.…”
Section: Discussionmentioning
confidence: 99%
“…In this sense, it is appropriate to remind the known model of oscillator with the "retarded argument" (Suarez and Schopf, 1988;Boutle et al, 2007) which quite truthfully describes a nonlinear dynamics of temperature oscillations (the ∆T anomalies) of the EL Nino current at annual time scale and in the modified form looks like:…”
Section: Discussionmentioning
confidence: 99%
“…(30) describes the strong positive feedback with the framework of the ocean-atmosphere system; the second term limits the growth of unstable perturbations of ocean temperature; b is the constant parameter; the fourth term emulates the motion of equatorial "trapped" waves (the Rossby "latent" waves) through the Pacific ocean, which after elastic reflection on the western continental boundary return (as the Kelvin waves) along the equator to the central part of the Pacific ocean with the time delay ∆; the fifth term Υ(t) describes the continuous changes of ocean surface average temperature in the course of year year; the sixth term (ℜ≈5°С/100 years) emulates the global warming; ξ(t) is the white noise of Gaussian type with zero mean (〈ξ(t)〉=0) and standard deviation λ (Suarez and Schopf, 1988;Boutle et al, 2007).…”
Section: Discussionmentioning
confidence: 99%
“…[19] where two sub-regions of the Pacific was incorporated in the model. Specifically, these models mimicked the coupling of regions along the equator, where one expects varying self-delay coupling strengths in the sub-regions, as well as varying (possibly strong) delay times [18]. We will first describe this coupled model in detail, and then review the patterns emerging in this class of models, as obtained in Ref.…”
Section: Introductionmentioning
confidence: 99%
“…1 has been scaled by k, temperature by b/k. The dimensionless constants α = A/k and δ = k∆ [18]. This model allows multiple steady states and when these fixed points become unstable, self-sustained oscillations emerge.…”
Section: Introductionmentioning
confidence: 99%