An Additional Analysis of Inertial Oscillations on the Continental Shelf
An Additional Analysis of Inertial Oscillations on the Continental Shelf
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DOI：
10.1007/978-1-4615-6648-9_15
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发表时间：
1983
期刊：
影响因子：
--
通讯作者：
C. Millot;C. Moulin
中科院分区：
文献类型：
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作者：
C. Millot;C. Moulin
用理论模型和大量时间序列的谱分析研究了大陆架的惯性振荡(Millot和Crepon，1981)；包括温跃层在内的特定深度区间的平均温度被认为代表了惯性频率手中内波的幅度。为了更好地估计由这些波引起的垂直位移，我们考虑了垂直温度梯度。这样的分析改进了已有的一些结果的精度，将该方法推广到几乎均匀层的测量，增加了理论的可靠性。
Inertial oscillations on the continental shelf have been studied with a theoretical model and spectral analysis of numerous time series (Millot and Crepon, 1981); the mean temperature over a specific depth interval including the thermocline was supposed to be representative of the amplitude of the internal waves in the inertial frequency hand. To estimate better the vertical displacements due to these waves, we take into account the vertical temperature gradient. Such an analysis improves the accuracy of some of the results already obtained, the method is extended to measurements in almost homogeneous layers, and the reliability of the theory is increased.