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首页> 外文期刊>The Cryosphere >Scoring Antarctic surface mass balance in climate models to refine future projections
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Scoring Antarctic surface mass balance in climate models to refine future projections

机译:在气候模型中评分南极表面质量平衡,以改善未来的预测

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An increase in Antarctic Ice Sheet (AIS) surface mass balance (SMB) has the potential to mitigate future sea level rise that is driven by enhanced solid ice discharge from the ice sheet. For climate models, AIS SMB provides a difficult challenge, as it is highly susceptible to spatial, seasonal, and interannual variability. Here we use a reconstructed data set of AIS snow accumulation as “true” observational data, to evaluate the ability of the CMIP5 and CMIP6 suites of models in capturing the mean, trends, temporal variability, and spatial variability in SMB over the historical period (1850–2000). This gives insight into which models are most reliable for predicting SMB into the future. We found that the best scoring models included the National Aeronautics and Space Administration (NASA) GISS model and the Max Planck Institute (MPI) for Meteorology's model for CMIP5, as well as one of the Community Earth System Model v2 (CESM2) models and one MPI model for CMIP6. Using a scoring system based on SMB mean value, trend, and temporal variability across the AIS, as well as spatial SMB variability, we selected a subset of the top 10th percentile of models to refine 21st century (2000–2100) AIS-integrated SMB projections to 2274? ± ?282?Gt?yr ?1 , 2358? ± ?286?Gt?yr ?1 , and 2495? ± ?291?Gt?yr ?1 for Representative Concentration Pathways (RCPs) 2.6, 4.5, and 8.5, respectively. We also reduced the spread in AIS-integrated mean SMB by 79?%, 79?%, and 74?% in RCPs 2.6, 4.5, and 8.5, respectively. Notably, we find that there is no improvement from CMIP5 to CMIP6 in overall score. In fact, CMIP6 performed slightly worse on average compared to CMIP5 at capturing the aforementioned SMB criteria. Our results also indicate that model performance scoring is affected by internal climate variability (particularly the spatial variability), which is illustrated by the fact that the range in overall score between ensemble members within the CESM1 Large Ensemble is comparable to the range in overall score between CESM1 model simulations within the CMIP5 model suite. We also find that a higher horizontal resolution does not yield to a conclusive improvement in score.
机译:南极冰盖(AIS)表面质量平衡(SMB)的增加具有减轻未来的海平面上升,这是由冰盖增强的固体冰放电驱动的。对于气候模型,AIS SMB提供了艰难的挑战,因为它非常容易受到空间,季节性和际变化的影响。在这里,我们使用一个重建的数据集AIS雪积累作为“真实”观察数据,以评估模型5和CMIP6套件在历史时期中捕获SMB中的平均值,趋势,时间变异性和空间变异性的能力( 1850-2000)。这为预测SMB预测到未来,这提供了最可靠的洞察力。我们发现,最佳评分模型包括全国航空航天局(NASA)GISS模型和MAX CLACK研究所(MPI)用于CMIP5的模型,以及一个社区地球系统模型V2(CESM2)模型之一和一个CMIP6的MPI模型。使用基于SMB的SMB平均值,趋势和时间变异性的评分系统,以及空间SMB可变性,我们选择了第10位模型的子集,优化21世纪(2000-2100)AIS-Integrated SMB投影到2274? ±282?GT?YR?1,2358? ±286?gt?1和2495?对于代表性浓度途径(RCPS)2.6,4.5和8.5,分别为±291〜291〜291?1。我们还将AIS-Integry平均值SMB的涂抹减少了79?%,79℃,分别为RCPS 2.6,4.5和8.5的74倍。值得注意的是,我们发现CMIP5到CMIP6的总成绩没有改善。实际上,与CMIP5在捕获上述SMB标准时,CMIP6平均略差。我们的结果还表明,模型性能评分受到内部气候变异性的影响(特别是空间变异性),这是由于CESM1大型集合内集合成员之间的总分数的范围与总分之间的范围相当的事实说明了CMIP5模型套件内的CESM1模型模拟。我们还发现更高的水平分辨率不会产生得分的结论性。

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