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Development and evaluation of a new regionalcoupled atmosphere-ocean model in the North Seaand Baltic Sea

机译:北海和波罗的海区域海洋耦合新模型的开发和评估

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摘要

A new regional coupled model system for the North Sea and the Baltic Sea is developed, which is composed ofthe regional setup of ocean model NEMO, the Rossby Centre regional climate model RCA4, the sea ice modelLIM3 and the river routing model CaMa-Flood. The performance of this coupled model system is assessed usinga simulation forced with ERA-Interim reanalysis data at the lateral boundaries during the period 19792010.Compared to observations, this coupled model system can realistically simulate the present climate. Since theactive coupling area covers the North Sea and Baltic Sea only, the impact of the ocean on the atmosphere overEurope is small. However, we found some local, statistically significant impacts on surface parameters like 2mair temperature and sea surface temperature (SST). A precipitation-SST correlation analysis indicates that bothcoupled and uncoupled models can reproduce the airsea relationship reasonably well. However, the coupledsimulation gives slightly better correlations even when all seasons are taken into account. The seasonalcorrelation analysis shows that the airsea interaction has a strong seasonal dependence. Strongest discrepanciesbetween the coupled and the uncoupled simulations occur during summer. Due to lack of airsea interaction, inthe Baltic Sea in the uncoupled atmosphere-standalone run the correlation between precipitation and SST is toosmall compared to observations, whereas the coupled run is more realistic. Further, the correlation analysisbetween heat flux components and SST tendency suggests that the coupled model has a stronger correlation. Ouranalyses show that this coupled model system is stable and suitable for different climate change studies.
机译:开发了一种新的北海和波罗的海区域耦合模型系统,该系统由海洋模型NEMO,罗斯比中心区域气候模型RCA4,海冰模型LIM3和河道模型CaMa-Flood的区域设置组成。该耦合模型系统的性能是通过在19792010年期间使用ERA-Interim再分析数据在横向边界上强制进行的模拟来评估的。由于活动耦合区仅覆盖北海和波罗的海,因此海洋对整个欧洲大气的影响很小。但是,我们发现对表面参数(如2气温和海面温度(SST))有一些局部的,统计学上显着的影响。降水与海表温度的相关性分析表明,耦合模型和非耦合模型都可以较好地再现气海关系。但是,即使将所有季节都考虑在内,耦合模拟也可以提供更好的相关性。季节相关分析表明,气海相互作用具有强烈的季节依赖性。耦合模拟和非耦合模拟之间的最大差异发生在夏季。由于缺乏气海相互作用,在波罗的海的非耦合大气独立运行中,降水和海表温度之间的相关性与观测值相比太小,而耦合运行则更为现实。此外,热通量分量与SST趋势之间的相关性分析表明,耦合模型具有更强的相关性。我们的分析表明,这种耦合模型系统是稳定的,适用于不同的气候变化研究。

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