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    Convective Adjustment and Thermohaline Excitability

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 004::page 481
    Author:
    Cessi, Paola
    DOI: 10.1175/1520-0485(1996)026<0481:CAATE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Welander's flip?flop model exhibits oscillations when forced by stochastic white noise (with zero mean) even in the region of parameters where the deterministic system has a globally stable fixed point. Perturbations away from the attracting solutions decay exponentially in time, without any oscillation. Thus, the oscillation that appears when the system is stochastically forced is not related to an eigenfrequency of the linearized system. The characteristics of this noise-induced oscillation are contrasted with those obtained when the damped harmonic oscillator is forced stochastically. In the case of a stochastically forced damped harmonic oscillator the spectral peak coincides with the frequency of the oscillator, and the amplitude of the oscillations is proportional to the strength of the noise. In the stochastically forced flip-flop model the amplitude of the oscillations is independent of the strength of the noise and the spectral peak moves to lower frequencies as the amplitude of the noise is reduced. Moreover, for noise below a critical threshold, no spectral peak is obtained. The flip?flop model shares four characteristics with the thermohaline oscillations observed in OGCMs: The freshwater flux determines whether the system oscillates or settles into a steady state. The period of the oscillations is very sensitive to the freshwater flux and becomes arbitrarily long near the transition from steady to periodic behavior. The oscillations are of finite amplitude even just past the threshold value of the freshwater flux that separates periodic behavior from a steady equilibrium. One extremum of the oscillation excursion is close to the value of the steady state that exists below the threshold for transition. When the deterministic system reaches a steady state, oscillations can be excited by adding a stochastic component to the freshwater flux. The period of the resulting oscillations decreases with increasing noise amplitude, while the amplitude of the oscillations is insensitive to the amplitude of the noise.
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      Convective Adjustment and Thermohaline Excitability

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    contributor authorCessi, Paola
    date accessioned2017-06-09T14:51:59Z
    date available2017-06-09T14:51:59Z
    date copyright1996/04/01
    date issued1996
    identifier issn0022-3670
    identifier otherams-28496.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165618
    description abstractWelander's flip?flop model exhibits oscillations when forced by stochastic white noise (with zero mean) even in the region of parameters where the deterministic system has a globally stable fixed point. Perturbations away from the attracting solutions decay exponentially in time, without any oscillation. Thus, the oscillation that appears when the system is stochastically forced is not related to an eigenfrequency of the linearized system. The characteristics of this noise-induced oscillation are contrasted with those obtained when the damped harmonic oscillator is forced stochastically. In the case of a stochastically forced damped harmonic oscillator the spectral peak coincides with the frequency of the oscillator, and the amplitude of the oscillations is proportional to the strength of the noise. In the stochastically forced flip-flop model the amplitude of the oscillations is independent of the strength of the noise and the spectral peak moves to lower frequencies as the amplitude of the noise is reduced. Moreover, for noise below a critical threshold, no spectral peak is obtained. The flip?flop model shares four characteristics with the thermohaline oscillations observed in OGCMs: The freshwater flux determines whether the system oscillates or settles into a steady state. The period of the oscillations is very sensitive to the freshwater flux and becomes arbitrarily long near the transition from steady to periodic behavior. The oscillations are of finite amplitude even just past the threshold value of the freshwater flux that separates periodic behavior from a steady equilibrium. One extremum of the oscillation excursion is close to the value of the steady state that exists below the threshold for transition. When the deterministic system reaches a steady state, oscillations can be excited by adding a stochastic component to the freshwater flux. The period of the resulting oscillations decreases with increasing noise amplitude, while the amplitude of the oscillations is insensitive to the amplitude of the noise.
    publisherAmerican Meteorological Society
    titleConvective Adjustment and Thermohaline Excitability
    typeJournal Paper
    journal volume26
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1996)026<0481:CAATE>2.0.CO;2
    journal fristpage481
    journal lastpage491
    treeJournal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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