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Internal gravity waves in the energy and flux budget turbulence-closure theory for shear-free stably stratified flows

机译:用于剪切稳定分层流动的能量和通量预算湍流理论中的内部重力波

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We have advanced the energy and flux budget turbulence closure theory that takes into account a two-way coupling between internal gravity waves (IGWs) and the shear-free stably stratified turbulence. This theory is based on the budget equation for the total (kinetic plus potential) energy of IGWs, the budget equations for the kinetic and potential energies of fluid turbulence, and turbulent fluxes of potential temperature for waves and fluid flow. The waves emitted at a certain level propagate upward, and the losses of wave energy cause the production of turbulence energy. We demonstrate that due to the nonlinear effects more intensive waves produce more strong turbulence, and this, in turn, results in strong damping of IGWs. As a result, the penetration length of more intensive waves is shorter than that of less intensive IGWs. The anisotropy of the turbulence produced by less intensive IGWs is stronger than that caused by more intensive waves. The low-amplitude IGWs produce turbulence consisting up to 90% of turbulent potential energy. This resembles the properties of the observed high-altitude tropospheric strongly anisotropic (nearly two-dimensional) turbulence.
机译:我们具有先进的能量和助焊剂预算湍流理论,其考虑了内部重力波(IGWS)与无剪切稳定分层湍流之间的双向耦合。该理论基于IGWS的总(动力学加电位)能量的预算方程,用于流体湍流的动力学和潜在能量的预算方程,以及波浪和流体流动的潜在温度的湍流通量。在一定水平发射的波向上传播,波动能量损失导致湍流能量的产生。我们证明,由于非线性效应更加强烈的波浪产生更强烈的湍流,而这反过来导致IGWS的强烈阻尼。结果,更强烈的波的渗透长度比不太强化的IGWS更短。由更密集的IGW产生的湍流的各向异性比由更强烈的波浪引起的湍流强。低振幅IGWS产生湍流,该湍流高达90%的湍流势能。这类似于观察到的高空对流层强烈各向异性(几乎二维)湍流的性质。

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