斜压海洋涡旋基于协变量的随机参数化

N. Verheul, J. Viebahn, D. Crommelin
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引用次数: 8

摘要

在这项研究中,我们研究了一种基于协变量的随机方法来参数化理想的风驱动海洋环流标准模型中未解决的湍流过程。我们专注于垂直粗粒度而不是水平粗粒度,这样我们就避免了水平粗粒度的微妙困难。相应的涡强迫有独特的定义,并且与斜压不稳定有明确的物理解释。我们建议通过从斜压参考模型数据中得到的涡强迫的条件概率分布函数抽样来模拟斜压涡强迫。这些条件概率分布函数在这里通过从离散参考值中均匀抽样来近似。我们详细分析了随机参数化的不同性能取决于涡强迫是否取决于合适的流动相关协变量或时间延迟协变量,或两者兼而有之。结果表明,我们的非高斯、非线性方法能够准确地再现参考斜压模型的流函数、能量学和熵的前四个统计矩和时空相关性。
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Covariate-based stochastic parameterization of baroclinic ocean eddies
Abstract In this study we investigate a covariate-based stochastic approach to parameterize unresolved turbulent processes within a standard model of the idealised, wind-driven ocean circulation. We focus on vertical instead of horizontal coarse-graining, such that we avoid the subtle difficulties of horizontal coarsegraining. The corresponding eddy forcing is uniquely defined and has a clear physical interpretation related to baroclinic instability.We propose to emulate the baroclinic eddy forcing by sampling from the conditional probability distribution functions of the eddy forcing obtained from the baroclinic reference model data. These conditional probability distribution functions are approximated here by sampling uniformly from discrete reference values. We analyze in detail the different performances of the stochastic parameterization dependent on whether the eddy forcing is conditioned on a suitable flow-dependent covariate or on a timelagged covariate or on both. The results demonstrate that our non-Gaussian, non-linear methodology is able to accurately reproduce the first four statistical moments and spatial/temporal correlations of the stream function, energetics, and enstrophy of the reference baroclinic model.
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