Application of the Spectral Nudging on Global Tides Towards a Global Total Water Level Prediction System

T. Kodaira, N. Bernier, K. Thompson
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引用次数: 2

Abstract

With the long-term goal of developing an ensemble forecast system for coastal flooding, we are developing a dynamically-based, numerical model of the global ocean. The model is based on the NEMO framework and has been used to predict global tides and surges in previous studies. This study focuses on the optimization of the joint prediction of both tides and surges, the two main components of total water level that cause coastal flooding. To improve the predictions of the tide we use a modified form of “spectral nudging”. We show this leads to significant improvements in the prediction of the M2 tide in the open ocean, and also in the shallow regions closer to shore where the model is not nudged. The median value of the vector difference of the tidal amplitude based on sea level observations and a data-assimilative model, and the predictions of our ocean model, is reduced from 11.2 cm to 2.66 cm by the nudging. The improvement deteriorates significantly however if additional tidal constituents are included in the model (most notably S2). This is explained in terms of spectral leakage between tidal bands associated with the nudging methodology and a straightforward solution is proposed.
全球潮汐的光谱微推在全球总水位预报系统中的应用
我们的长期目标是开发一个沿海洪水的综合预报系统,我们正在开发一个基于动态的全球海洋数值模型。该模型基于NEMO框架,并在之前的研究中被用于预测全球潮汐和涨潮。本研究的重点是潮汐和浪涌联合预测的优化,这是引起沿海洪水的总水位的两个主要组成部分。为了改进对潮汐的预测,我们使用了一种改进形式的“谱轻推”。我们表明,这导致了开阔海域M2潮汐预测的显著改进,也导致了模型未被推动的靠近海岸的浅水区域M2潮汐预测的显著改进。基于海平面观测和数据同化模式以及我们的海洋模式预测的潮汐振幅矢量差的中位数在推力作用下从11.2 cm减小到2.66 cm。然而,如果在模型中包括额外的潮汐成分(最明显的是S2),则改善显着恶化。这是解释在潮汐带之间的频谱泄漏与微推方法,并提出了一个直接的解决方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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