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A Unifying Perspective on Transfer Function Solutions to the Unsteady Ekman Problem

机译:对不稳定EKMAN问题的转移功能解决方案的统一视角

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The unsteady Ekman problem involves finding the response of the near-surface currents to wind stress forcing under linear dynamics. Its solution can be conveniently framed in the frequency domain in terms of a quantity that is known as the transfer function, the Fourier transform of the impulse response function. In this paper, a theoretical investigation of a fairly general transfer function form is undertaken with the goal of paving the way for future observational studies. Building on earlier work, we consider in detail the transfer function arising from a linearly-varying profile of the vertical eddy viscosity, subject to a no-slip lower boundary condition at a finite depth. The horizontal momentum equations, rendered linear by the assumption of horizontally uniform motion, are shown to transform to a modified Bessel’s equation for the transfer function. Two self-similarities, or rescalings that each effectively eliminate one independent variable, are identified, enabling the dependence of the transfer function on its parameters to be more readily assessed. A systematic investigation of asymptotic behaviors of the transfer function is then undertaken, yielding expressions appropriate for eighteen different regimes, and unifying the results from numerous earlier studies. A solution to a numerical overflow problem that arises in the computation of the transfer function is also found. All numerical code associated with this paper is distributed freely for use by the community.
机译:不稳定的EKMAN问题涉及在线性动力学下发现近表面电流对风力应力强制进行响应。它的解决方案可以在频域中方便地在频域中框架,其数量被称为传递函数,脉冲响应函数的傅里叶变换。在本文中,对一个相当一般的转移函数形式的理论调查是为了铺平未来观察研究的目标。在早期的工作中,我们考虑详细考虑从垂直涡粘度的线性变化轮廓引起的传递函数,在有限深度下受到无滑动下边界条件的影响。通过假设水平均匀的运动,水平动量方程被呈现线性,被示出为转换为改进的贝塞尔的传递函数的等式。识别每个有效地消除一个独立变量的两个自相似度或重构,从而实现传递函数对其参数的依赖性更容易评估。然后进行对转移功能的渐近行为的系统调查,产生适合于十八个不同制度的表达,并统一许多早期研究的结果。还发现了在计算传递函数的计算中出现的数值溢出问题的解决方案。与本文相关联的所有数值代码都自由地分发以供社区使用。

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