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Tropical extra-tropical thermocline water mass exchanges in the Community Climate Model v.3 Part I: the Atlantic Ocean

机译:社区气候模式第3部分中的热带热带外温跃层水质交换第一部分:大西洋

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The climatological annual mean tropical-extra-tropical pathways ofthermocline waters in the Atlantic Ocean are investigated with the NCAR CCSMnumerical coupled model. Results from three numerical experiments areanalyzed: Two are fully coupled runs with different spatial resolution (T42and T85) for the atmospheric component. The third numerical experiment is anocean-only run forced by NCEP winds and fluxes. Results show that thedifferent atmospheric resolutions have a significant impact on the subductionpathways in the Atlantic because of how the wind field is represented. Thesesimulation results also show that the water subducted at the subtropicsreaching the EUC is entirely from the South Atlantic. The coupled modelability to simulate the STCs is discussed.
机译:利用NCAR CCSM数值耦合模型研究了大西洋大西洋上热带海水的气候年平均热带-热带关系。分析了三个数值实验的结果:两个是完全耦合的运行,其中大气成分具有不同的空间分辨率(T42和T85)。第三个数值实验是在NCEP的风和通量的作用下,仅在海洋上运行。结果表明,由于风场的表示方式不同,大气分辨率对大西洋的俯冲路径有重要影响。这些模拟结果还表明,在亚热带地区到达EUC的俯冲水完全来自南大西洋。讨论了模拟STC的耦合建模能力。

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