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An application of a data assimilation method based on the diffusion stochastic process theory using altimetry data in Atlantic

机译:基于扩散随机过程理论的高程数据在数据同化方法中的应用

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At data assimilation (DA) method based on the application of the diffusion stochastic process theory, particularly, of the Fokker-Planck equation, is considered. The method was introduced in the previous works; however, it is substantially modified and extended to the multivariate case in the current study. For the first time, the method is here applied to the assimilation of sea surface height anomalies (SSHA) into the Hybrid Coordinate Ocean Model (HYCOM) over the Atlantic Ocean. The impact of assimilation of SSHA is investigated and compared with the assimilation by an Ensemble Optimal Interpolation method (EnOI). The time series of the analyses produced by both assimilation methods are evaluated against the results from a free model run without assimilation. This study shows that the proposed assimilation technique has some advantages in comparison with EnOI analysis. Particularly, it is shown that it provides slightly smaller error and is computationally efficient. The method may be applied to assimilate other data such as observed sea surface temperature and vertical profiles of temperature and salinity.
机译:在基于扩散随机过程理论(尤其是Fokker-Planck方程)的应用的数据同化(DA)方法中。该方法是在以前的工作中介绍的。但是,在当前的研究中,对它进行了实质性的修改并将其扩展到多变量情况。这是该方法首次在大西洋上将海面高度异常(SSHA)同化为混合坐标海洋模型(HYCOM)。研究了SSHA同化的影响,并通过集成最优内插法(EnOI)与同化进行了比较。两种同化方法产生的分析的时间序列是根据没有同化的自由模型运行的结果进行评估的。研究表明,与EnOI分析相比,拟议的同化技术具有一些优势。特别地,显示出它提供了稍微小的误差并且在计算上是有效的。该方法可用于吸收其他数据,例如观测到的海面温度以及温度和盐度的垂直剖面。

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