Lagrangian analysis of submesoscale flows from sparse data using Gaussian Process Regression for field reconstruction

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
H.M. Aravind , Tamay M. Özgökmen , Michael R. Allshouse
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引用次数: 0

Abstract

Lagrangian analyses of oceanic flows provide insight into the various transport pathways in the ocean. This analysis typically relies on a dense set of trajectories that can be computed using high-resolution velocity fields, which are often not available during field experiments. Instruments like drifters and floats are often employed to overcome the limitations imposed by satellite- and radar-based velocity fields, to understand the transport pathways in the ocean. However, the sparsity in available drifter-trajectory data proves prohibitive to obtaining a comprehensive map of the Lagrangian characteristics of the underlying flow. To circumvent these issues, we use Gaussian Process Regression (GPR) to obtain velocity fields from sparse drifter data to generate synthetic trajectories and subsequently estimate two Lagrangian metrics, FTLE and dilation rate. A detailed error analysis is performed for drifter clusters deployed within various dynamical regions in the analytic Bickley jet system. The uncertainties in velocity reconstruction obtained from the GPR method, averaged along particle trajectories, locate Lagrangian confidence regions that are applicable both to synthetic trajectories and the dilation rate field. A sensitivity analysis reveals the role played by factors such as the spatial sampling density and temporal resolution of the drifter data, as well as the effect of position uncertainty as a result of GPS inaccuracy. The method is then applied to the drifter data from the Lagrangian Submesoscale Experiment in 2016 to locate convergent filaments. The results present a marked improvement over direct estimation of area-averaged dilation rates using drifter clusters.
利用高斯过程回归对稀疏数据进行亚中尺度流动的拉格朗日分析
拉格朗日对海洋流动的分析提供了对海洋中各种运输途径的洞察。这种分析通常依赖于密集的轨迹集,这些轨迹集可以使用高分辨率的速度场来计算,这在现场实验中通常是不可用的。像漂浮器和浮标这样的仪器经常被用来克服基于卫星和雷达的速度场所施加的限制,以了解海洋中的运输路径。然而,可用的漂流轨迹数据的稀疏性证明难以获得下伏流的拉格朗日特征的综合图。为了避免这些问题,我们使用高斯过程回归(GPR)从稀疏漂移数据中获得速度场,以生成合成轨迹,并随后估计两个拉格朗日指标,FTLE和膨胀率。对分析型毕克利射流系统中不同动力区域内的漂移簇进行了详细的误差分析。GPR方法得到的速度重建中的不确定性沿粒子轨迹平均,定位于拉格朗日置信区域,该区域既适用于合成轨迹,也适用于膨胀率场。灵敏度分析揭示了漂移数据的空间采样密度和时间分辨率等因素的作用,以及GPS不精度导致的位置不确定性的影响。然后将该方法应用于2016年拉格朗日亚中尺度实验的漂移数据,以定位收敛细丝。结果表明,与使用漂移簇直接估计面积平均膨胀率相比,有明显的改进。
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来源期刊
Ocean Modelling
Ocean Modelling 地学-海洋学
CiteScore
5.50
自引率
9.40%
发文量
86
审稿时长
19.6 weeks
期刊介绍: The main objective of Ocean Modelling is to provide rapid communication between those interested in ocean modelling, whether through direct observation, or through analytical, numerical or laboratory models, and including interactions between physical and biogeochemical or biological phenomena. Because of the intimate links between ocean and atmosphere, involvement of scientists interested in influences of either medium on the other is welcome. The journal has a wide scope and includes ocean-atmosphere interaction in various forms as well as pure ocean results. In addition to primary peer-reviewed papers, the journal provides review papers, preliminary communications, and discussions.
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