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A multi-column vertical mixing scheme to parameterize the heterogeneity of oceanic conditions under sea ice

机译:海冰下海洋条件非均质性的多列垂直混合方案

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The heterogeneity of ocean surface conditions associated with a spatially variable sea ice cover needs to be represented in models in order to represent adequately mixed layer processes and the upper ocean density structure. This study assesses the sensitivity of the ocean-sea ice model NEMO-LIM to a subgrid-scale representation of ice-ocean interactions. The sea ice component includes an ice thickness distribution, which provides heterogeneous surface buoyancy fluxes and stresses. A multi-column ocean scheme is developed to take them explicitly into account, by computing convection and turbulent vertical mixing separately in the open water/lead fraction of grid cells and below each ice thickness category. For the first time in a three-dimensional simulation, the distinct temperature and salinity profiles of the ocean columns are allowed to be maintained over several time steps. It is shown that the model response is highly sensitive to the homogenization time scale between the columns. If the latter are laterally mixed with time scales shorter than 10 h, subgrid-scale effects exist but the mean state is practically unaffected. For longer mixing time scales, in both hemispheres, the main impacts are reductions in under-ice mean mixed layer depths and in the summer melt of sea ice, following decreased oceanic heat flux at the ice base. Large changes in the open water temperature in summer suggest that the scheme could trigger important feedback processes in coupled simulations. (C) 2016 Elsevier Ltd. All rights reserved.
机译:需要在模型中表示与空间变化的海冰覆盖量相关的海洋表面状况的非均质性,以便表示充分的混合层过程和上部海洋密度结构。这项研究评估了海冰模型NEMO-LIM对冰网相互作用的亚网格规模表示的敏感性。海冰成分包括冰厚度分布,这提供了不均匀的表面浮力通量和应力。通过在网格单元的开放水/铅分数中且在每个冰厚度类别以下分别计算对流和湍流垂直混合,开发了一种多列海洋方案以明确考虑它们。在三维模拟中,第一次允许在多个时间步骤中保持海柱的不同温度和盐度分布。结果表明,模型响应对色谱柱之间的均质化时间尺度高度敏感。如果后者横向混合且时间尺度短于10 h,则存在亚网格尺度效应,但平均状态实际上不受影响。对于更长的混合时间尺度,在两个半球,主要影响是冰底平均混合层深度的减少以及夏季海冰融化的减少,这是由于冰基的海洋热通量下降所致。夏季开放水温的巨大变化表明,该方案可能会在耦合模拟中触发重要的反馈过程。 (C)2016 Elsevier Ltd.保留所有权利。

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