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首页> 外文期刊>Journal of Advances in Modeling Earth Systems >The Flexible Global Ocean‐Atmosphere‐Land System Model Grid‐Point Version 3 (FGOALS‐g3): Description and Evaluation
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The Flexible Global Ocean‐Atmosphere‐Land System Model Grid‐Point Version 3 (FGOALS‐g3): Description and Evaluation

机译:灵活的全球海洋气氛 - 陆地系统模型网格点版本3(FGOALS-G3):描述和评估

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This paper introduces the Flexible Global Ocean‐Atmosphere‐Land System Model: Grid‐Point Version 3 (FGOALS‐g3) and evaluates its basic performance based on some of its participation in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) experiments. Our results show that many significant improvements have been achieved by FGOALS‐g3 in terms of climatological mean states, variabilities, and long‐term trends. For example, FGOALS‐g3 has a small (?0.015°C/100?yr) climate drift in 700‐yr preindustrial control (piControl) runs and smaller biases in climatological mean variables, such as the land/sea surface temperatures (SSTs) and seasonal soil moisture cycle, compared with its previous version FGOALS‐g2 during the historical period. The characteristics of climate variabilities, for example, Madden‐Julian oscillation (MJO) eastward/westward propagation ratios, spatial patterns of interannual variability of tropical SST anomalies, and relationship between the East Asian Summer Monsoon and El Ni?o–Southern Oscillation (ENSO), are well captured by FGOALS‐g3. In particular, the cooling trend of globally averaged surface temperature during 1940–1970, which is a challenge for most CMIP3 and CMIP5 models, is well reproduced by FGOALS‐g3 in historical runs. In addition to the external forcing factors recommended by CMIP6, anthropogenic groundwater forcing from 1965 to 2014 was incorporated into the FGOALS‐g3 historical runs. Plain Language Summary The sixth phase of the Coupled Model Intercomparison Project (CMIP6) is a crucial support for the sixth Assessment Report of Intergovernmental Panel on Climate Change (IPCC AR6) and will also provide important foundation for research in climate change in the next few years. This paper gives the description of FGOALS‐g3 model, its experiment configures, and the experiments conducted according to the experimental design of CMIP6 and evaluates the preliminary performance of model simulation. This work offers references to CMIP6 data users and provides enormous output data sets for assessing and understanding climate change.
机译:本文介绍了灵活的全球海洋气氛 - 陆地系统模型:网格点版本3(FGoALS-G3)并根据其参与耦合模型离心项目(CMIP6)实验的第六阶段来评估其基本性能。我们的研究结果表明,FGOALS-G3在气候均值,可白性能力和长期趋势方面取得了许多重大改进。例如,FGOALS-G3在700 yr的预工业控制(皮卡尔罗尔)中的气候漂移有一个小(?0.015°C / 100?YR)气候漂移,在气候平均变量中运行和较小的偏见,例如陆地/海面温度(SST)和季节性水分循环,与其先前的历史期间FGoAls-G2相比。气候变量的特点,例如Madden-Julian振荡(MJO)向东/向西传播比,热带SST异常年间变异性的空间模式,以及东亚夏季季风和EL NI的关系,o-Southern振荡(ENSO ),由FGOALS-G3拍摄。特别是,1940-1970期间的全球平均表面温度的冷却趋势是对大多数CMIP3和CMIP5模型的挑战,由FGOALS-G3在历史运行中良好地再现。除了CMIP6推荐的外部矫正因素外,1965年至2014年的人为地下​​水迫使迫使FGOALS-G3历史跑步。普通语言摘要耦合型号的第六阶段耦合型号互相项目(CMIP6)是对政府间气候变化小组(IPCC AR6)的第六次评估报告的关键支持(IPCC AR6),也将为未来几年的气候变化研究提供重要基础。本文提供了FGOALS-G3模型的描述,其实验配置,以及根据CMIP6的实验设计进行的实验,并评估模型模拟的初步性能。这项工作提供了对CMIP6数据用户的引用,并提供巨大的输出数据集,用于评估和理解气候变化。
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