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- W3141570688 abstract "从海冰形成的盐水排水在海洋在极的海洋混合和 halocline 的季节的变化起一个关键作用。盐水排水和它的导致的传送对流的水平规模比当盐水排水在一个格子房间上被平均时，一个气候模型格子和一个模型趋于生产混合的假海洋的小得多。一个二列的海洋格子(TCOG ) 计划用联合的海冰海洋模型设定明确地解决在社区地球系统模型(CESM ) 被实现有或没有盐水拒绝的在一个模型格子的二亚列的不同垂直混合。有盐水拒绝的格子的部分被测试在一样的大气的数据从 1978 ～ 2009 强迫的一系列敏感模型跑等于铅部分或一个小经常的数字。模型结果与从 29 冰的观察相比在从 2004 ～ 2009 的北极海洋盆的拴住的剖析程序(ITP ) 。与用一个常规海洋格子的控制跑相比， TCOG 模拟在咸度显示出模型错误的一致减小并且混合了层深度(MLD ) 。用为盐水拒绝的一个小经常的部分格子的模型被发现与观察生产最好的模型比较，显示盐水排水的水平规模与海冰盖子相比是很小的并且比铅部分甚至小。比得上用盐水拒绝 parameterization 计划的模型， TCOG 在咸度完成了更多的改进但是在 MLD 类似。" @default.
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- W3141570688 date "2015-01-01" @default.
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- W3141570688 title "Sensitivity study of subgrid scale ocean mixing under sea ice using a two-column ocean grid in climate model CESM" @default.
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