由位置不确定性引起的物理约束协方差膨胀

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Yicun Zhen, V. Resseguier, B. Chapron
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引用次数: 1

摘要

摘要在“位置不确定性”概念的激励下,最初在msammin(2014)中引入,寻求一种方案来扰动状态变量在每个预测时间步长的“位置”。进一步考虑Brenier定理(Brenier, 1991),断言同一域上两个正密度场的差可以用运输图表示,我们证明了扰动一致地定义了原始PDE的随机偏微分方程(SPDE)。结果是,在每个时间步上,一定数量的量(由用户决定)是守恒的。值得注意的是,SALT(随机平流由李氏输运;Holm, 2015)和LU (location uncertainty;Memin, 2014;Resseguier et al., 2017a)设置可以从该摄动方案中恢复。尽管如此,它还是提供了更广泛的适用性,因为它不明确地依赖于拉格朗日力学或牛顿的力定律。为了说明,给出了一个随机版本的浅水热方程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Physically constrained covariance inflation from location uncertainty
Abstract. Motivated by the concept of “location uncertainty”, initially introduced in Mémin (2014), a scheme is sought to perturb the “location” of a state variable at every forecast time step. Further considering Brenier's theorem (Brenier, 1991), asserting that the difference of two positive density fields on the same domain can be represented by a transportation map, we demonstrate that the perturbations consistently define a stochastic partial differential equation (SPDE) from the original PDE. It ensues that certain quantities, up to the user, are conserved at every time step. Remarkably, derivations following both the SALT (stochastic advection by Lie transport; Holm, 2015) and LU (location uncertainty; Mémin, 2014; Resseguier et al., 2017a) settings can be recovered from this perturbation scheme. Still, it offers broader applicability since it does not explicitly rely on Lagrangian mechanics or Newton's laws of force. For illustration, a stochastic version of the thermal shallow water equation is presented.
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来源期刊
Nonlinear Processes in Geophysics
Nonlinear Processes in Geophysics 地学-地球化学与地球物理
CiteScore
4.00
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: Nonlinear Processes in Geophysics (NPG) is an international, inter-/trans-disciplinary, non-profit journal devoted to breaking the deadlocks often faced by standard approaches in Earth and space sciences. It therefore solicits disruptive and innovative concepts and methodologies, as well as original applications of these to address the ubiquitous complexity in geoscience systems, and in interacting social and biological systems. Such systems are nonlinear, with responses strongly non-proportional to perturbations, and show an associated extreme variability across scales.
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