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Internal tide acoustic tomography: reliability of the normal modes expansion as a possible basis for solving the inverse problem

机译:内潮声层析成像:正常模式扩展的可靠性可作为解决反问题的基础

摘要

Using hydrodynamic and thermodynamic equations appropriate for modellinginternal tides, one can predict the current and temperature distributions associatedwith the ocean's dynamic modes. Comparing such predictions with observations from theINTIMATE'96 experiment, we nd a high degree of correlation between the rst 3 theoretically calculated dynamic modes and corresponding empirical orthogonal functions (EOF's) derived from an ensemble of temperature and current pro les. The implications are twofold.First, this implies that the dominant variability in the INTIMATE'96 experiment isindeed associated with internal tides. Secondly, it suggests that in future tidal experiments a theoretically generated basis may be used as e ectively as an EOF basis (which requires more extensive oceanographic measurements). We have also used the set of dynamic modes to simulate the e ect of the tides on acoustic propagation to understand the relative importance of the usual surface tide (barotropic) and the internal (baroclinic) tides.
机译:使用适用于内部潮汐建模的流体动力学和热力学方程,可以预测与海洋动力模式相关的电流和温度分布。将这些预测与INTIMATE'96实验的观察结果进行比较,我们发现在前3种理论计算的动态模式与相应的经验正交函数(EOF)之间的高度相关性,这些正交函数是由温度和电流曲线的集合得出的。其含义是双重的。首先,这意味着INTIMATE'96实验的主要变异性确实与内部潮汐有关。其次,它表明在将来的潮汐实验中,理论上产生的基础可以有效地用作EOF基础(这需要更广泛的海洋学测量)。我们还使用了一组动态模式来模拟潮汐对声音传播的影响,以了解通常的表面潮汐(正压)和内部潮汐(斜压)的相对重要性。

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