温跃层
WKB近似
内波
波长
物理
唤醒
常量(计算机编程)
邻里(数学)
分层流
机械
经典力学
数学分析
分层流
数学
光学
湍流
地质学
量子力学
海洋学
计算机科学
程序设计语言
标识
DOI:10.1080/03091927108236052
摘要
Abstract The internal waves produced by either a moving body or the collapsing wake behind a moving body in a stratified fluid are calculated asymptotically (at large distances behind the source) on the hypotheses of small disturbances, the Boussinesq approximation, and the slender-body approximation (the transverse dimensions of the body and wake are small compared with the wavelengths of the significant internal waves). Explicit results are given for two, complementary models: (a) a constant-N model, in which the density gradient is constant and (b) a thin-thermocline model, in which the density gradient peaks sharply in a thin layer and is elsewhere negligible. The internal-wave spectrum is continuous in (a) and discrete in (b); however, only the dominant mode is included in the explicit results given for (b). A WKB solution also is given for a thermocline model. This approximation does not give an adequate representation of the dominant mode but does provide estimates of the contributions of the higher modes that are neglected in the thin-thermocline model. These contributions are typically negligible relative to that of the dominant mode in the neighbourhood of the maximum, free-surface disturbance.
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