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从专家那里获取关于气候快速变化可能性的信息。

Eliciting information from experts on the likelihood of rapid climate change.

作者信息

Arnell Nigel W, Tompkins Emma L, Adger W Neil

机构信息

Tyndall Centre for Climate Change Research, School of Geography, University of Southampton, Highfield, Southampton, SO17, 1BJ, UK.

出版信息

Risk Anal. 2005 Dec;25(6):1419-31. doi: 10.1111/j.1539-6924.2005.00689.x.

Abstract

The threat of so-called rapid or abrupt climate change has generated considerable public interest because of its potentially significant impacts. The collapse of the North Atlantic Thermohaline Circulation or the West Antarctic Ice Sheet, for example, would have potentially catastrophic effects on temperatures and sea level, respectively. But how likely are such extreme climatic changes? Is it possible actually to estimate likelihoods? This article reviews the societal demand for the likelihoods of rapid or abrupt climate change, and different methods for estimating likelihoods: past experience, model simulation, or through the elicitation of expert judgments. The article describes a survey to estimate the likelihoods of two characterizations of rapid climate change, and explores the issues associated with such surveys and the value of information produced. The surveys were based on key scientists chosen for their expertise in the climate science of abrupt climate change. Most survey respondents ascribed low likelihoods to rapid climate change, due either to the collapse of the Thermohaline Circulation or increased positive feedbacks. In each case one assessment was an order of magnitude higher than the others. We explore a high rate of refusal to participate in this expert survey: many scientists prefer to rely on output from future climate model simulations.

摘要

所谓快速或突然的气候变化所带来的威胁因其潜在的重大影响而引发了公众的广泛关注。例如,北大西洋热盐环流或西南极冰盖的崩塌,可能会分别对气温和海平面产生灾难性影响。但这种极端气候变化发生的可能性有多大呢?真的有可能估算其可能性吗?本文回顾了社会对快速或突然气候变化可能性的需求,以及估算可能性的不同方法:过去的经验、模型模拟或通过专家判断的引出。本文描述了一项旨在估算快速气候变化两种特征可能性的调查,并探讨了与此类调查相关的问题以及所产生信息的价值。这些调查基于因在突变气候变化的气候科学方面具有专业知识而被挑选出来的关键科学家。大多数调查受访者认为快速气候变化发生的可能性较低,原因要么是热盐环流的崩塌,要么是正反馈增加。在每种情况下,有一种评估比其他评估高出一个数量级。我们探讨了此次专家调查中较高的拒绝参与率:许多科学家更愿意依赖未来气候模型模拟的输出结果。

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