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Statistical and dynamical properties of covariant lyapunov vectors in a coupled atmosphere-ocean model—multiscale effects, geometric degeneracy, and error dynamics

机译:大气-海洋耦合模型中协变lyapunov向量的统计和动力学性质—多尺度效应,几何退化和误差动力学

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摘要

We study a simplified coupled atmosphere-ocean model using the formalism of covariant Lyapunov vectors (CLVs), which link physically-based directions of perturbations to growth/decay rates. The model is obtained via a severe truncation of quasi-geostrophic equations for the two fluids, and includes a simple yet physically meaningful representation of their dynamical/thermodynamical coupling. The model has 36 degrees of freedom, and the parameters are chosen so that a chaotic behaviour is observed. There are two positive Lyapunov exponents (LEs), sixteen negative LEs, and eighteen near-zero LEs. The presence of many near-zero LEs results from the vast time-scale separation between the characteristic time scales of the two fluids, and leads to nontrivial error growth properties in the tangent space spanned by the corresponding CLVs, which are geometrically very degenerate. Such CLVs correspond to two different classes of ocean/atmosphere coupled modes. The tangent space spanned by the CLVs corresponding to the positive and negative LEs has, instead, a non-pathological behaviour, and one can construct robust large deviations laws for the finite time LEs, thus providing a universal model for assessing predictability on long to ultra-long scales along such directions. Interestingly, the tangent space of the unstable manifold has substantial projection on both atmospheric and oceanic components. The results show the difficulties in using hyperbolicity as a conceptual framework for multiscale chaotic dynamical systems, whereas the framework of partial hyperbolicity seems better suited, possibly indicating an alternative definition for the chaotic hypothesis. They also suggest the need for an accurate analysis of error dynamics on different time scales and domains and for a careful set-up of assimilation schemes when looking at coupled atmosphere-ocean models.
机译:我们使用协变李雅普诺夫向量(CLV)的形式主义研究简化的大气-海洋模型,该模型将基于物理的扰动方向链接到增长/衰减率。该模型是通过对两种流体的拟地转方程进行严格截断而获得的,并且包括了其动力/热力学耦合的简单但在物理上有意义的表示。该模型具有36个自由度,并且选择了参数以观察到混沌行为。有两个正Lyapunov指数(LE),十六个负LE和18个接近零的LE。许多接近零的LE的存在是由于两种流体的特征时间尺度之间的巨大时间尺度间隔而导致的,并导致由相应CLV跨越的切线空间中的非平凡误差增长特性,这些CLV在几何上非常退化。这样的CLV对应于海洋/大气耦合模式的两个不同类别。相反,CLV对应于正负LE的切线空间具有非病理学行为,并且可以为有限时间LE构造稳健的大偏差定律,从而提供了一种通用模型,用于评估从长到超的LE的可预测性-沿着这样的方向长鳞片。有趣的是,不稳定歧管的切线空间在大气和海洋成分上都有大量投影。结果表明,使用双曲性作为多尺度混沌动力学系统的概念框架存在困难,而部分双曲性框架似乎更适合,这可能表明了对混沌假设的另一种定义。他们还建议有必要在不同的时间尺度和域上对误差动态进行准确的分析,并在研究耦合的海洋-海洋模型时需要仔细设置同化方案。

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