首页> 外文期刊>Oceanologia >New coupled atmosphere-ocean-ice system COSMO-CLM/NEMO: assessing air temperature sensitivity over the North and Baltic Seas
【24h】

New coupled atmosphere-ocean-ice system COSMO-CLM/NEMO: assessing air temperature sensitivity over the North and Baltic Seas

机译:新的大气-海洋-冰层耦合系统COSMO-CLM / NEMO:评估北海和波罗的海的气温敏感性

获取原文
       

摘要

This paper introduces a newly established coupled atmosphere-ocean-ice system with the regional climate model COSMO-CLM and the ocean-sea-ice model NEMO for the North and Baltic Seas. These two models are linked via the OASIS3 coupler. Experiments with the new coupled system and with the stand-alone COSMO-CLM model forced by ERA-Interim re-analysis data over the period from 1985 to 1994 for the CORDEX Europe domain are carried out. The evaluation results of the coupled system show 2-m temperature biases in the range from -2.5 to 3K. Simulated 2-m temperatures are generally colder in the coupled than in the uncoupled system, and temperature differences vary by season and space. The coupled model shows an improvement compared with the stand-alone COSMO-CLM in terms of simulating 2-m temperature. The difference in 2-m temperature between the two experiments are explained as downwind cooling by the colder North and Baltic Seas in the coupled system.
机译:本文介绍了一个新建立的大气-海洋-冰体耦合系统,其区域气候模型为COSMO-CLM,而北海和波罗的海的海洋-海冰模型为NEMO。这两个模型通过OASIS3耦合器链接。在1985年至1994年期间,针对新的耦合系统以及独立的COSMO-CLM模型进行了实验,这些模型是由ERA-Interim重新分析的数据在1985年至1994年期间针对CORDEX Europe域进行的。耦合系统的评估结果显示2-m温度偏差在-2.5至3K的范围内。耦合系统中模拟的2米温度通常比非耦合系统中的温度低,并且温差会随季节和空间而变化。与独立的COSMO-CLM相比,耦合模型在模拟2 m温度方面显示出改进。两次实验之间2 m温度的差异被解释为耦合系统中北海和波罗的海较冷的顺风冷却。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号