首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Three-dimensional hindcast simulation of internal soliton propagationin the Asian Seas International Acoustics Experiment area
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Three-dimensional hindcast simulation of internal soliton propagationin the Asian Seas International Acoustics Experiment area

机译:亚洲海洋国际声学实验区内部孤子传播的三维后预报模拟

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摘要

Internal solitary waves referred to as solitons are common occurrences in the SouthChina Sea. The Asian Seas International Acoustics Experiment (ASIAEX) experimentwas carried out in April-May 2001 to perform measurements on these solitons, which areoften highly energetic, having isopycnal displacements well over 100 m and phasespeeds greater than 2.5 m/s. Of particular interest is the interaction of a soliton with thesloping shelf bottom that occurs as the soliton shoals to water depths less than its waveheight. Observations during the experiment show that at such shallow depths, a solitonundergoes strong refraction and transformation. In this article, we present hindcastsimulation of a particular soliton observed during the experiment, using a fully nonlinear,nonhydrostatic, three-dimensional model and the actual bathymetry from the ASIAEXarea. The computation begins with the soliton at a distance about 100 km from the shelfand obtains the propagation and evolution of the soliton over the shelf-slope. Thethree-dimensional hindcast is able to reproduce the refraction of the soliton propagationobserved during the experiment as well as the propagation speed and direction in therange observed. The final nonlinear transformation of the soliton from symmetrical toskewed elongated waveform is also obtained in the model consistent with theobservations. The hindcast simulation reveals that the relative position of soliton'svorticity core to the local water depth is a crucial indicator of the onset of transformationand formation of elevation waves.
机译:内部孤立波(称为孤子)在南中国海很常见。 2001年4月至5月进行了亚洲海洋国际声学实验(ASIAEX)实验,对这些孤子进行了测量,这些孤子的等渗位移远超过100 m,相速度大于2.5 m / s,它们通常是高能的。特别关注的是孤子与倾斜的搁板底部之间的相互作用,这是由于孤子向浅水深浅至小于其波高的水深而发生的。实验期间的观察表明,在如此浅的深度,孤子经历了强烈的折射和变形。在本文中,我们将使用全非线性,非静水的三维模型和来自ASIAEXarea的实际测深法,对实验期间观察到的特定孤子进行后验模拟。计算从距架子约100 km处的孤子开始,并获得孤子在架子斜坡上的传播和演化。三维后验能够再现实验过程中观察到的孤子传播的折射,以及在观察范围内的传播速度和方向。在与观测值一致的模型中,还获得了孤子从对称的偏斜细长波形的最终非线性变换。后验模拟表明,孤子涡核的相对位置与局部水深的关系是高程波转换和形成的关键指标。

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