Construction of a wavefront model for internal solitary waves and its application in the Northern South China Sea

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Zijian Cui , Chujin Liang , Feilong Lin , Shuangshuang Chen , Tao Ding , Beifeng Zhou , Weifang Jin , Wankang Yang
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引用次数: 0

Abstract

Internal solitary waves (ISWs) play a crucial role in the development of various physical and biological processes, and numerous high-precision two-dimensional or three-dimensional numerical models have been developed to simulate the generation and propagation processes of ISWs. However, these numerical models, especially when simulating the interaction between ISWs and ocean circulation, require substantial computational resources. This burden can make it challenging to apply them in real-time or short-term forecasting scenarios. In this study, we propose a new numerical model for ISWs by combining traditional one-dimensional ISW theory with wave refraction theory. The proposed model resolves the issues of ray crossing and divergence, which are commonly encountered in traditional refraction models, by employing equally spaced grids along the wave crest line. As a result, this model is capable of simulating the far-field propagation of ISWs. This model enables rapid prediction of the vertical structure and wave crest morphology of ISWs in specific current fields and at given time frames, and it is utilized to investigate the characteristics and propagation of ISWs generated by the nonlinear steepening of internal tide (IT) in the South China Sea. Comparative analysis with satellite imagery demonstrates the model's accurate representation of ISW processes and phenomena, such as wave crest line discontinuities, diffraction, and wave‒wave interactions when passing through Dongsha Island. Furthermore, propagation time estimates based on this model have errors of ±0.98 h (1σ) over which the ISWs are observed by a mooring system, and the average time difference is 0.81 h

内孤波波前模型的构建及其在南海北部的应用
内孤波(ISW)在各种物理和生物过程的发展中起着至关重要的作用,目前已开发出许多高精度的二维或三维数值模型来模拟内孤波的产生和传播过程。然而,这些数值模型,特别是在模拟 ISW 与海洋环流之间的相互作用时,需要大量的计算资源。这种负担会使其在实时或短期预报场景中的应用面临挑战。在本研究中,我们将传统的一维 ISW 理论与波浪折射理论相结合,提出了一种新的 ISW 数值模型。所提出的模型通过沿波峰线采用等间距网格,解决了传统折射模型中常见的射线交叉和发散问题。因此,该模型能够模拟 ISW 的远场传播。该模型可快速预测特定海流场和给定时间段内 ISW 的垂直结构和波峰形态,并用于研究南海内潮非线性陡变产生的 ISW 的特征和传播。与卫星图像的对比分析表明,该模型准确地再现了 ISW 的过程和现象,如通过东沙岛时的波峰线不连续、衍射和波浪相互作用。此外,根据该模型估算的传播时间误差为±0.98 h (1σ),其中系泊系统观测到的 ISW 时间误差平均为 0.81 h。
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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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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