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Impacts of Changes of External Forcings from CMIP5 to CMIP6 on Surface Temperature in FGOALS-g2

机译:CMIP5对FGOALS-G2的表面温度对CMIP5至CMIP6对CMIP6的影响

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External forcings among the different phases of the Coupled Model Intercomparison Project (CMIP) vary considerably, but their impacts have not been extensively investigated yet. This study compares the impacts of CMIP5 and CMIP6 forcings on model stability and the 20th-century global warming and El-Ni?o Southern Oscillation (ENSO) based on the Pre-Industrial control (PI-control) and historical runs of the Flexible Global Ocean–Atmosphere–Land System Model: Grid-point Version 2 (FGOALS-g2). Results indicate that CMIP6 forcings result in a larger climate drift and a lower climatological global average surface temperature (GAST) than those of CMIP5 in PI-control runs. In historical runs, stronger 20th-century warming trends occur during the periods 1910-1940 and 1970-2005 using CMIP6 forcings, which are closer to the HadCRUT than those of the CMIP5 forcings simulation. A stronger spurious warming trend in the CMIP6 results in an evolution of GAST that is less consistent with the HadCRUT dataset than that in the CMIP5 during 1940-1970. Among all forcings, GHGs and aerosol forcings play the dominant roles in differences in GAST, particularly in the Northern Hemisphere. In both the PI-control and historical runs, a larger ENSO amplitude and smaller seasonality are simulated in CMIP6 than in CMIP5.
机译:耦合型号相互校准项目(CMIP)的不同阶段之间的外部强制差异很大,但它们的影响尚未得到广泛调查。本研究比较了CMIP5和CMIP6强调对模型稳定和20世纪的全球变暖和EL-NI的影响,基于工业预工业控制(PI-Control)和灵活的全球历史跑步的南方振荡(ENSO)海洋气氛 - 陆地系统模型:网格点版本2(FGoAls-G2)。结果表明,CMIP6强制导致较大的气候漂移和低气候全局平均表面温度(GAST)比PI控制运行中的CMIP5更低。在历史的运行中,使用CMIP6强制期间,在1910年至1940年和1970 - 2005年期间发生了强大的20世纪的变暖趋势,这些趋势比CMIP6强制更接近CMIP5强制仿真。 CMIP6中的一个更强烈的杂散变暖趋势导致加速度的演变,与Hadcrut DataSet不那么一致,而不是CMIP5在1940-1970期间。在所有强迫中,温室气体和气溶胶强迫症中的差异在北半球的差异中发挥着差异。在PI控制和历史运行中,在CMIP6中模拟了较大的ENSO幅度和较小的季节性而不是CMIP5。

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