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利用观测与多气候模型模拟约束未来气候预测

研究问题
如何结合历史观测与多个气候模型共享的涌现关系,约束本世纪末北极变暖预测,并区分不同来源的不确定性?
方法与思路
作者结合十三个气候模型与观测数据,建立基于模型与地球系统共可交换表示的分层贝叶斯框架,并纳入内部及自然变异。
材料陈述的贡献
摘要称历史观测可降低部分北极地区的预测变暖幅度和不确定性,并指出忽略气候模型内部变异可能导致预测偏差。
阅读关注点
应核对共可交换表示的含义、涌现关系如何进入模型、两类变异的区分,以及区域预测变化对先验和模型设定的敏感性。
阅读边界
仅据 OpenAlex 索引摘要,稿件版本未注明,不能推断刊本变化;摘要未说明具体先验和模型诊断,区域结果不能直接推广至整个北极。

原文摘要

Numerical climate models are used to project future climate change due to both anthropogenic and natural causes. Differences between projections from different climate models are a major source of uncertainty about future climate. Emergent relationships shared by multiple climate models have the potential to constrain our uncertainty when combined with historical observations. We combine projections from 13 climate models with observational data to quantify the impact of emergent relationships on projections of future warming in the Arctic at the end of the 21st century. We propose a hierarchical Bayesian framework based on a coexchangeable representation of the relationship between climate models and the Earth system. We show how emergent constraints fit into the coexchangeable representation, and extend it to account for internal variability simulated by the models and natural variability in the Earth system. Our analysis shows that projected warming in some regions of the Arctic may be more than 2 °C lower and our uncertainty reduced by up to 30% when constrained by historical observations. A detailed theoretical comparison with existing multi-model projection frameworks is also provided. In particular, we show that projections may be biased if we do not account for internal variability in climate model predictions. Supplementary materials for this article, including a standardized description of the materials available for reproducing the work, are available as an online supplement.

笔记与分组
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