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首页> 外文期刊>Climatic Change >Towards Bayesian hierarchical inference of equilibrium climate sensitivity from a combination of CMIP5 climate models and observational data
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Towards Bayesian hierarchical inference of equilibrium climate sensitivity from a combination of CMIP5 climate models and observational data

机译:从CMIP5气候模型和观察数据的组合到贝叶斯平衡气候敏感性的贝叶斯分层推理

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摘要

Despite decades of research, large multi-model uncertainty remains about the Earth's equilibrium climate sensitivity to carbon dioxide forcing as inferred from state-of-the-art Earth system models (ESMs). Statistical treatments of multi-model uncertainties are often limited to simple ESM averaging approaches. Sometimes models are weighted by how well they reproduce historical climate observations. Here, we propose a novel approach to multi-model combination and uncertainty quantification. Rather than averaging a discrete set of models, our approach samples from a continuous distribution over a reduced space of simple model parameters. We fit the free parameters of a reduced-order climate model to the output of each member of the multi-model ensemble. The reduced-order parameter estimates are then combined using a hierarchical Bayesian statistical model. The result is a multi-model distribution of reduced-model parameters, including climate sensitivity. In effect, the multi-model uncertainty problem within an ensemble of ESMs is converted to a parametric uncertainty problem within a reduced model. The multi-model distribution can then be updated with observational data, combining two independent lines of evidence. We apply this approach to 24 model simulations of global surface temperature and net top-of-atmosphere radiation response to abrupt quadrupling of carbon dioxide, and four historical temperature data sets. Our reduced order model is a 2-layer energy balance model. We present probability distributions of climate sensitivity based on (1) the multi-model ensemble alone and (2) the multi-model ensemble and observations.
机译:尽管有数十年的研究,但大量的多模型不确定性仍然是迫使地球平衡气候敏感性,因为从最先进的地球系统模型(ESMS)推断出来的二氧化碳。多模型不确定性的统计处理通常限于简单的ESM平均方法。有时,模型是重量他们重现历史气候观测的程度。在这里,我们提出了一种新的多模型组合和不确定性量化的方法。我们的方法在简单模型参数的减少空间上连续分布,我们的方法样本而不是平均离散的模型。我们将下降秩序的气候模型的自由参数符合多模型集合的每个成员的输出。然后使用分层贝叶斯统计模型组合降低的参数估计。结果是减少模型参数的多模型分布,包括气候敏感性。实际上,ESMS集合内的多模型不确定性问题在减少模型中转换为参数不确定性问题。然后可以通过观察数据更新多模型分布,组合两个独立的证据。我们将这种方法应用于全局表面温度的24个模型模拟,净全体辐射响应响应二氧化碳的突然四倍,四个历史温度数据集。我们的减少阶模型是2层能量平衡模型。我们基于(1)单独的多模型集合和(2)多模型集合和观察,呈现气候敏感度的概率分布。

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