Potential for bias in effective climate sensitivity from state-dependent energetic imbalance

B. Sanderson, M. Rugenstein
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引用次数: 1

Abstract

Abstract. To estimate equilibrium climate sensitivity from a simulation where a step change in carbon dioxide concentrations is imposed, a common approach is to linearly extrapolate temperatures as a function of top-of-atmosphere energetic imbalance to estimate the equilibrium state (“effective climate sensitivity”). In this study, we find that this estimate may be biased in some models due to state-dependent energetic leaks. Using an ensemble of multi-millennial simulations of climate model response to a constant forcing, we estimate equilibrium climate sensitivity through Bayesian calibration of simple climate models which allow for responses from subdecadal to multi-millennial timescales. Results suggest potential biases in effective climate sensitivity in the case of particular models where radiative tendencies imply energetic imbalances which differ between pre-industrial and quadrupled CO2 states, whereas for other models even multi-thousand-year experiments are insufficient to predict the equilibrium state. These biases draw into question the utility of effective climate sensitivity as a metric of warming response to greenhouse gases and underline the requirement for operational climate sensitivity experiments on millennial timescales to better understand committed warming following a stabilization of greenhouse gases.
依赖状态的能量失衡对有效气候敏感性的潜在偏差
摘要为了从二氧化碳浓度阶跃变化的模拟中估计平衡气候敏感性,一种常见的方法是将温度作为大气顶部能量不平衡的函数进行线性外推,以估计平衡状态(“有效气候敏感性”)。在这项研究中,我们发现由于状态相关的能量泄漏,这种估计可能在某些模型中有偏差。利用气候模式对恒定强迫响应的千年模拟集合,我们通过简单气候模式的贝叶斯校准来估计平衡气候敏感性,这些模式允许从年代际到千年时间尺度的响应。结果表明,在辐射趋势暗示工业化前和四倍二氧化碳状态之间能量不平衡的特定模式中,有效气候敏感性存在潜在偏差,而对于其他模式,即使是几千年的实验也不足以预测平衡状态。这些偏差使人们对有效气候敏感性作为温室气体变暖响应度量的效用产生疑问,并强调需要在千年时间尺度上进行气候敏感性实验,以便更好地了解温室气体稳定后持续变暖的情况。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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