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Dynamically evolving Gaussian spatial fields

机译:动态演化的高斯空间场

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We discuss general non-stationary spatio-temporal surfaces that involve dynamics governed by velocity fields. The approach formalizes and expands previously used models in analysis of satellite data of significant wave heights. We start with homogeneous spatial fields. By applying an extension of the standard moving average construction we obtain models which are stationary in time. The resulting surface changes with time but is dynamically inactive since its velocities, when sampled across the field, have distributions centered at zero. We introduce a dynamical evolution to such a field by composing it with a dynamical flow governed by a given velocity field. This leads to non-stationary models. The models are extensions of the earlier discretized autoregressive models which account for a local velocity of traveling surface. We demonstrate that for such a surface its dynamics is a combination of dynamics introduced by the flow and the dynamics resulting from the covariance structure of the underlying stochastic field. We extend this approach to fields that are only locally stationary and have their parameters varying over a larger spatio-temporal horizon.
机译:我们讨论了涉及由速度场控制的动力学的一般非平稳时空表面。该方法形式化并扩展了先前使用的模型,用于分析具有重要波高的卫星数据。我们从同质空间场开始。通过应用标准移动平均线构造的扩展,我们可以获得时间上固定的模型。生成的表面随时间变化,但由于在整个野外采样时其速度都集中于零,因此它是动态不活动的。通过将其与由给定速度场控制的动态流组成,我们将动态演化引入这种场。这导致了非平稳模型。该模型是较早的离散自回归模型的扩展,后者说明了行进表面的局部速度。我们证明,对于这样的表面,其动力学是由流动引入的动力学和由基础随机场的协方差结构产生的动力学的组合。我们将此方法扩展到仅局部静止且其参数在较大的时空范围内变化的场。

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