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UK Global Ocean GO6 and GO7: a traceable hierarchy of model resolutions

机译:英国全球海洋GO6和GO7:一种可追踪的模型分辨率层次结构

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Versions 6 and 7 of the UK Global Ocean configuration (known as GO6 and GO7) will form the ocean components of the Met Office GC3.1 coupled model and UKESM1 earth system model to be used in CMIP61 simulations. The label “GO6” refers to a traceable hierarchy of three model configurations at nominal 1, 1∕4 and 1/12° resolutions. The GO6 configurations are described in detail with particular focus on aspects which have been updated since the previous version (GO5). Results of 30-year forced ocean-ice integrations with the 1/4° model are presented, in which GO6 is coupled to the GSI8.1 sea ice configuration and forced with CORE22 fluxes. GO6-GSI8.1 shows an overall improved simulation compared to GO5-GSI5.0, especially in the Southern Ocean where there are more realistic summertime mixed layer depths, a reduced near-surface warm and saline biases, and an improved simulation of sea ice. The main drivers of the improvements in the Southern Ocean simulation are tuning of the vertical and isopycnal mixing parameters. Selected results from the full hierarchy of three resolutions are shown. Although the same forcing is applied, the three models show large-scale differences in the near-surface circulation and in the short-term adjustment of the overturning circulation. The GO7 configuration is identical to the GO6 1/4° configuration except that the cavities under the ice shelves are opened. Opening the ice shelf cavities has a local impact on temperature and salinity biases on the Antarctic shelf with some improvement in the biases in the Weddell Sea.
机译:英国全球海洋配置(称为GO6和GO7)的版本6和7将形成MET Office GC3.1耦合模型和UKESM1地球系统模型的海洋组件,以用于CMIP61模拟。标签“GO6”是指标称1,1 / 4和1/12°分辨率的三种模型配置的可追踪层次结构。 GO6配置详细描述,特别侧重于自上一个版本(GO5)以来已经更新的方面。提出了30年的强制海洋冰集成,其中包括1/4°模型,其中GO6耦合到GSI8.1海冰配置并强制使用Core22助熔剂。 GO6-GSI8.1显示了与GO5-GSI5.0相比的整体改进的模拟,尤其是在南部海洋中,在南洋中有更具现实的夏季混合层深度,降低的近表面温热和盐水偏差,以及改善的海冰模拟。南洋仿真改进的主要驱动因素正在调整垂直和等离子体混合参数。显示了三个分辨率的完整层次结构的选定结果。虽然应用了相同的迫使,但这三种模型显示了近表面循环的大规模差异,并在倾覆循环的短期调节中进行了大规模的差异。 GO7配置与GO6 1/4°配置相同,不同之处在于打开冰架下的空腔。打开岩石架腔对南极架上的温度和盐度偏差有一定的影响,在楔子海中的偏差有所改善。
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