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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >The semi-diurnal cycle of dissipation in a ROFI: model-measurement comparisons
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The semi-diurnal cycle of dissipation in a ROFI: model-measurement comparisons

机译:ROFI中耗散的半日循环:模型与测量的比较

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The Liverpool Bay Region of Freshwater Influence in the Irish Sea exhibits strong horizontal gradients which interact with the dominant tidal flow. A 25 h series of measurements of the cycle of turbulent dissipation with the FLY dissipation profiler shows a strong asymmetry between ebb and flood which is associated with a cycle of increasing stratification on the ebb and progressive mixing on the flood which results in vertical homogeneity as high water is approached. At this time strong dissipation extends throughout the water column in contrast to the ebb when there is a near shutdown of dissipation in the upper half of the column, The cycle of stratification and dissipation is closely consistent for the two semi-diurnal tidal cycles observed. We have attempted to Simulate this situation, which involves a complex suite of processes including tidal straining and mixing, using a version of the k-epsilon closure scheme in a 1-d dynamical model which is forced by a combination of the observed tidal Row and horizontal temperature and salinity gradients. The latter were measured directly at the end of the observational series but, in order to focus on the cycle of dissipation, the correct reproduction of the temperature and salinity cycle can be assured by a nudging procedure which obliges the model temperature and salinity values to track the observations. With or without this procedure, the model gives a reasonable account of tire dissipation and its asymmetric behaviour on ebb and flood although nudging improves the timing of peak dissipation in the upper part of the water column near highwater. The model has also been used to examine the ratio of shear production (P/epsilon) and buoyancy inputs to dissipation (B/epsilon). The variation of these quantities over the tidal cycle confirms the important role of convective motions forced by tidal straining near the end of the flood phase of the tide. (C) 2002 Published by Elsevier Science Ltd. [References: 27]
机译:爱尔兰海的利物浦湾淡水影响区域表现出强烈的水平梯度,与主要的潮汐流相互作用。用FLY耗散廓线仪对湍流耗散周期进行的25小时系列测量显示,潮起潮落与洪水之间存在强烈的不对称性,这与潮起潮落分层增加和洪水上渐进混合的循环有关,这导致垂直均匀度很高接近水。这时,当水柱上半部的水流几乎停滞时,强烈的水散流遍及整个水柱。在观察到的两个半日潮汐周期中,分层和水散的周期非常一致。我们试图模拟这种情况,其中涉及一组复杂的过程,包括潮汐应变和混合,在一维动力学模型中使用k-ε封闭方案的一种版本,该模型由观测到的潮汐行和水平温度和盐度梯度。后者是在观测序列末尾直接测量的,但是,为了关注耗散的周期,可以通过微调程序来确保温度和盐度循环的正确再现,该程序必须使模型的温度和盐度值能够跟踪观察。不论是否使用此程序,该模型都可以合理地考虑轮胎耗散及其在潮起潮落时的不对称行为,尽管通过微调可以改善高水位附近水柱上部的峰值耗散时间。该模型还用于检查剪切力产生量(P /ε)和浮力输入与耗散量(B /ε)之比。这些量在潮汐周期中的变化证实了潮汐洪水潮临近末期,由潮汐应变强迫的对流运动的重要作用。 (C)2002由Elsevier Science Ltd.发布[参考:27]

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