Estimating ocean flow fields in 3D is a critical step in enabling the reliable operation of underwater gliders and other small, low-powered autonomous marine vehicles. Existing methods produce depth-averaged 2D layers arranged at discrete vertical intervals, but this type of estimation can lead to severe navigation errors. Based on the observation that real-world ocean currents exhibit relatively low velocity vertical components, we propose an accurate 3D estimator that extends our previous work in estimating 2D flow fields as a linear combination of basis flows. The proposed algorithm uses data from ensemble forecasting to build a set of 3D basis flows, and then iteratively updates basis coefficients using point measurements of underwater currents. We report results from experiments using actual ensemble forecasts and synthetic measurements to compare the performance of our method to the direct 3D extension of the previous work. These results show that our method produces estimates with dramatically lower error metrics, with and without measurement noise.
翻译:估计3D的海洋流场是使水下滑翔机和其他小型、低功率自主海洋飞行器可靠运行的关键步骤。现有方法产生以离散垂直间隔排列的深度平均2D层,但这种估计可能导致严重的导航误差。根据现实世界洋流显示出相对低速垂直构件的观察,我们建议了精确的3D估计法,以扩大我们以前估计2D流域的工作,作为基础流线性组合。拟议的算法利用从混合预测获得的数据来建立一套3D基流,然后利用水下洋流的点测量进行迭代更新基系数。我们报告通过实验的结果,用实际的集成预测和合成测量将我们方法的性能与先前工作的直接3D扩展进行比较。这些结果表明,我们的方法产生估计数时差得非常低,有测量噪声,而且没有测量噪音。