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Induction in arbitrarily shaped oceans VI, oceans of variable depth

机译:诱导任意形状的海洋VI,深度可变的海洋

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摘要

We present calculations of t he electric currents induced in a model ocean by the 24 hr Sq variation. The model has realistic bathymetry and represents a further step of a consistent approach to oceanic induction in which we have introduced various complexities in order of priority. The solution obtained is compared with our previously published results for the case of an ocean of realistic shape and uniform depth. It is found that the major shelf-seas considerably modify the pattern of elect ric current circu­ lation in the oceans of the southern hemisphere. The consistent nature of the method of matched outer and inner expansions which we have used is also discussed. It seems probable that other methods, not limited to finding an outer solution and consequently more complicated, will at best only produce an outer solution since, in practice, the relatively coarse mesh necessarily used in the computation of realistic global problems precludes a fine resolution of the coastal bathymetry. Finally , the meaning of the internal and external Legendre coefficients and their relationship to Sq over the oceans is briefly discussed.
机译:我们提出了24小时平方变化在模型海洋中感应出的电流的计算。该模型具有逼真的测深法,代表了一种一致的海洋归纳方法的进一步步骤,在该方法中,我们按优先级顺序引入了各种复杂性。对于真实形状和均匀深度的海洋,将获得的解与我们以前发表的结果进行比较。已经发现,主要的陆架海大大改变了南半球海洋中的电流环流模式。我们还讨论了匹配的外部和内部扩展方法的一致性。似乎其他方法(不仅限于寻找外部解,因此更加复杂)似乎最多只会产生外部解,因为在实践中,在计算实际全局问题时必须使用相对较粗的网格,无法精确求解沿海测深。最后,简要讨论了内部和外部勒让德系数的含义以及它们与海洋Sq的关系。

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