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Spin-up from rest in a stratified fluid: boundary flows

机译:在分层流体中从静止加速旋转:边界流

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We present the results of an integrated experimental, numerical and theoretical examination of spin-up from rest of a stratified fluid. A vertical cylindrical container of radius R and height 2H containing fluid of viscosity v and characterized by a constant buoyancy frequency V is set impulsively to rotate about its symmetry axis with angular speed Omega = f/2. The characteristic Ekman number E = v/OmegaR(2) is small and the Schmidt number S = v/D-s (where D-s is the diffusivity of salt) is large. The investigation is focused on elucidating the initial stage of spin-up, which is characterized by an axisymmetric circulation driven by nonlinear Ekman layers adjoining the horizontal boundaries. Fluid is drawn by the boundary layers from the stationary, stratified interior and transported into corner regions. It is shown that the corner regions are restricted to a height of approximately 0.3Rf/N from the horizontal boundaries, above which the fluid remains unperturbed apart from that spun up by diffusion of momentum from the sidewall boundary. Two distinct regions thus emerge: rotating corner regions, and a quiescent stratified core. After a time 1.3/((EN)-N-1/2), the corner regions cover the bulk of the horizontal boundaries and the boundary layer suction is suppressed. Our study provides a framework for understanding the subsequent evolution of the spin-up process, which may be characterized by axisymmetry-breaking instabilities of the stratified core. [References: 37]
机译:我们提出了从其余分层流体中旋转产生的综合实验,数值和理论检验的结果。半径为R,高度为2H的垂直圆柱容器被冲动设置为绕其对称轴旋转,角速度为O,高度为2H,该流体的粘度为v,浮力频率为V,角速度为ωmega= f / 2。特征埃克曼数E = v / OmegaR(2)小,而施密特数S = v / D-s(其中D-s是盐的扩散率)大。该研究的重点是阐明自旋的初始阶段,该阶段的特征是轴对称环流是由与水平边界相邻的非线性埃克曼层驱动的。边界层从静止的分层内部抽取流体,并将其输送到拐角区域。示出了拐角区域被限制在距水平边界大约0.3Rf / N的高度上,在该高度之上,流体保持不受扰动,除了通过从侧壁边界动量的扩散而旋转的流体之外。因此出现了两个不同的区域:旋转角区域和静态分层核心。在时间1.3 /(((EN)-N-1 / 2))之后,拐角区域覆盖了大部分水平边界,并且边界层吸力得到抑制。我们的研究为理解自旋过程的后续发展提供了一个框架,其特征可能是分层核心的轴对称破坏不稳定性。 [参考:37]

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