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首页> 外文期刊>Journal of Applied Meteorology and Climatology >Probability-Weighted Ensembles of US County-Level Climate Projections for Climate Risk Analysis
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Probability-Weighted Ensembles of US County-Level Climate Projections for Climate Risk Analysis

机译:用于气候风险分析的美国县级气候预测的概率加权集合

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摘要

Quantitative assessment of climate change risk requires a method for constructing probabilistic time series of changes in physical climate parameters. Here, two such methods, surrogate/model mixed ensemble (SMME) and Monte Carlo pattern/residual (MCPR), are developed and then are applied to construct joint probability density functions (PDFs) of temperature and precipitation change over the twenty-first century for every county in the United States. Both methods produce likely (67% probability) temperature and precipitation projections that are consistent with the Intergovernmental Panel on Climate Change's interpretation of an equal-weighted Coupled Model Intercomparison Project phase 5 (CMIP5) ensemble but also provide full PDFs that include tail estimates. For example, both methods indicate that, under "Representative Concentration Pathway'' 8.5, there is a 5% chance that the contiguous United States could warm by at least 8 degrees C between 1981-2010 and 2080-99. Variance decomposition of SMME and MCPR projections indicates that background variability dominates uncertainty in the early twenty-first century whereas forcing-driven changes emerge in the second half of the twenty-first century. By separating CMIP5 projections into unforced and forced components using linear regression, these methods generate estimates of unforced variability from existing CMIP5 projections without requiring the computationally expensive use of multiple realizations of a single GCM.
机译:气候变化风险的定量评估需要一种方法来构建物理气候参数变化的概率时间序列。在这里,开发了两种这样的方法:替代/模型混合系综(SMME)和蒙特卡洛模式/残差(MCPR),然后将其用于构建二十一世纪温度和降水变化的联合概率密度函数(PDF)美国的每个县。两种方法都可能产生(67%概率)的温度和降水预测,这与政府间气候变化专门委员会对等加权耦合模型比较项目第5阶段(CMIP5)集合的解释是一致的,但也提供了包含尾部估计值的完整PDF。例如,这两种方法都表明,在“代表性浓度途径” 8.5中,连续的美国在1981-2010年至2080-99年间可能至少升温8摄氏度的可能性为5%。 MCPR预测表明,背景可变性在二十一世纪初占主导地位,而强迫驱动的变化则在二十一世纪下半叶出现,通过线性回归将CMIP5预测分为非强迫分量和强迫分量,这些方法可得出无需现有CMIP5预测的强制变化,而无需在计算上使用单个GCM的多种实现。

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