CMIP5 GCMs对北方冬季大气遥相关模态的未来模拟评价

E. Kristóf
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引用次数: 1

摘要

在本研究中,对耦合模式比对项目第5阶段(CMIP5)传播的7个gcm的RCP4.5和RCP8.5模拟输出应用模式检测方法,以确定欧洲中期天气预报中心(ECMWF)在ERA-20C再分析中检测到的大气遥相关模式是否会在CMIP5 gcm的未来预估中被观测到。将负极值法与接收机工作特征(ROC)曲线分析相结合的模式检测技术应用于北半球冬季500hpa气压水平的位势高度场。结果表明,在RCP4.5和RCP8.5情景下,2006-2035年、2021-2050年和2071-2100年期间,从ERA-20C再分析数据集中获得的1976-2005年期间的遥相关在大多数GCM输出中仍然可观测到。结果表明,大气内部变率是控制遥相关的主要因素,而不是辐射强迫的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of Future Simulations of the CMIP5 GCMs Concerning Boreal Wintertime Atmospheric Teleconnection Patterns
In this study, a pattern detection method is applied on the RCP4.5 and RCP8.5 simulation outputs of seven GCMs—disseminated by the Coupled Model Intercomparison Project Phase 5 (CMIP5)—to determine whether atmospheric teleconnection patterns detected in the ERA-20C reanalysis from the European Centre for Medium-Range Weather Forecasts (ECMWF) will be observable in the future projections of the CMIP5 GCMs. The pattern detection technique—which combines the negative extrema method and receiver operating characteristic (ROC) curve analysis—is used on the geopotential height field at the 500 hPa pressure level in wintertime, in the Northern Hemisphere. It was found that teleconnections obtained from the ERA-20C reanalysis dataset for the period of 1976–2005 remain observable in the majority of the GCM outputs under the RCP4.5 and RCP8.5 scenarios for the periods of 2006–2035, 2021–2050, and 2071–2100. The results imply that atmospheric internal variability is the major factor that controls the teleconnections rather than the impact of radiative forcing.
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