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在气候预测中的不确定性:原因,幅度和政策的影响

Uncertainties in Climate Forecasts: Causes, Magnitudes and Policy Implications
课程网址: http://videolectures.net/mitworld_schneider_ucf/  
主讲教师: Stephen Schneider
开课单位: 斯坦福大学
开课时间: 2013-03-28
课程语种: 英语
中文简介:
作为正在进行中的政府间气候变化专门委员会(IPCC)的主要研究人员之一,斯蒂芬施耐德(Stephen Schneider)致力于为气候变化讨论中的科学家制定适当的权限。他提醒政策制定者,科学家不能判定什么构成了全球气温的危险上升。“决定什么是危险的不是科学家的判断”,他必须为这些讨论制定精确的术语,并提供各种(大部分是悲观的)预测所依据的模型。全球讨论的核心是有争议的问题,即什么样的温度上升构成了“危险的人为干扰”(联合国简写为dai),以及在什么样的时间范围内。施耐德注意到,没有一个门槛低于正常值,高于正常值。“当某些物种濒临灭绝时,我们已经超过了临界点。”此外,将要发生的“损害”也有很大差别:北极海冰融化可能会使渔业每年节省5000万美元的较短路线,但它会破坏因纽特人的文化,因纽特人的文化已经建立了5000多年,or破坏北极熊生态系统。你如何在可比的货币计量中衡量这些?“在过去十年左右的时间里,施耐德和其他科学家试图为这些问题提供越来越复杂的答案,不仅运行了数千种气候模型,而且将剧烈气候变化的风险视为替代政策选择的一个功能。如果世界大气中二氧化碳含量比工业前水平翻一番,比如说每百万分之550,那么到2100年,气温会是多少,这将如何影响不同的地区、经济体和社会?最新的IPPC评估表明,我们可以预计气温会升高1.1-6.4摄氏度。施耐德说,决策者,本质上是风险管理者,很难接受这种不确定的预测,但最好的办法是在不同的场景中提供不同温度范围的可能性。rios。施耐德发现了一个最有用的装置来说明这种思维方式,那就是麻省理工学院的温室赌博轮盘赌,它描述了如果世界决定花费数万亿美元来稳定碳排放量在550 ppm,或者像往常一样继续商业活动,可能的温度升高。有了合理的全球政策,最有可能的结果是增加不超过1.5摄氏度。没有政策,预计增加2-2.5摄氏度。“你更愿意待在哪个世界?施耐德问道。
课程简介: As one of the lead researchers in the ongoing Intergovernmental Panel on Climate Change (IPCC), which informs the UN Framework Convention on Climate Change, Stephen Schneider has labored mightily to map out the appropriate purview for scientists in climate change discussions. He reminds policy makers that scientists can’t decree what constitutes a perilous increase in global temperatures. “It’s not a scientist’s judgment to decide what’s dangerous.” He must lay out precise terminology for these discussions, and provide the models on which the various (mostly dismal) forecasts are based. At the heart of the global discussion lie the contentious issues of what kind of rise in temperature constitutes “dangerous anthropogenic interference,” (DAI, in U.N. shorthand) and over what kind of time frame. Schneider notes that there is no threshold below which we’re OK, and above which we’re not. “We’ve already passed the threshold when some species are driven to extinction.” Also, the “damages that will occur are highly differential: melting Arctic sea ice will probably save the fishing industry $50 million a year in having shorter routes, but it will wreck the culture of the Inuits, established over 5,000 years, or destroy the polar bear ecosystem. How do you weigh those in comparable monetary metrics?” In successive passes over the last decade or so, Schneider and other scientists have attempted to provide increasingly sophisticated answers to these questions, not only running thousands of climate models but looking at the risk of drastic climate change as a function of alternative policy choices. If the world doubles the amount of carbon dioxide in the atmosphere over pre-industrial levels, say to 550 parts per million, what will temperatures be by 2100, and how will that impact different regions, economies, societies? The latest IPPC assessment shows that we can expect a temperature increase of anywhere from 1.1-6.4 degrees C. Decision makers, who are essentially risk managers, have difficulty accepting such an uncertain forecast, says Schneider, but the best that can be accomplished is to provide the likelihoods of different temperature ranges in varying scenarios. One of the most useful devices Schneider has found for illustrating this way of thinking is MIT’s Greenhouse Gamble roulette wheel, which depicts possible temperature increases should the world decide to spend the trillions of dollars necessary to stabilize carbon emissions at 550 ppm -- or pursue business as usual. With a rational global policy in place, the most likely outcome is an increase of no more than 1.5 degrees C. With no policy, expect a 2- 2.5 degree increase. “Which world would you rather be on?” asks Schneider.
关 键 词: 环境; 气候变化; 气候预测
课程来源: 视频讲座网
最后编审: 2020-04-24:chenxin
阅读次数: 69