The temperature–CO2 climate connection: an epistemological reappraisal of ice-core messages

IF 0.5 4区 哲学 Q4 GEOSCIENCES, MULTIDISCIPLINARY History of Geo- and Space Sciences Pub Date : 2021-05-26 DOI:10.5194/HGSS-12-97-2021
P. Richet
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Abstract

Abstract. As simply based on fundamental logic and on the concepts of cause and effect, an epistemological examination of the geochemical analyses performed on the Vostok ice cores invalidates the marked greenhouse effect on past climate usually assigned to CO2 and CH4. In agreement with the determining role assigned to Milankovitch cycles, temperature has, instead, constantly remained the long-term controlling parameter during the past 423 kyr, which, in turn, determined both CO2 and CH4 concentrations, whose variations exerted, at most, a minor feedback on temperature itself. If not refuted, the demonstration indicates that the greenhouse effect of CO2 on 20th century and today's climate remains to be documented, as already concluded from other evidence. The epistemological weakness of current simulations originates from the fact that they do not rely on any independent evidence for the influence of greenhouse gases on climate over long enough periods of time. The validity of models will, in particular, not be demonstrated as long as at least the most important features of climate changes, namely the glacial–interglacial transitions and the differing durations of interglacial periods, remain unaccounted for. Similarly, the constant 7 kyr time lag between temperature and CO2 decreases following deglaciation is another important feature that needs to be understood. Considered in this light, the current climate debate should be considered as being the latest of the great controversies that have punctuated the march of the Earth sciences, although its markedly differs from the preceding ones by its most varied social, environmental, economical and political ramifications.
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温度-二氧化碳气候联系:对冰芯信息的认识论重新评估
摘要简单地说,基于基本逻辑和因果概念,对沃斯托克冰芯进行的地球化学分析的认识论审查使通常归属于CO2和CH4的对过去气候的显著温室效应无效。在过去的423年中,温度一直是长期的控制参数,这与米兰科维奇循环的决定作用一致 kyr,这反过来又确定了CO2和CH4的浓度,其变化对温度本身的影响最大。如果不加以反驳,这一证据表明,二氧化碳对20世纪和当今气候的温室效应仍有待记录,正如其他证据所得出的结论一样。当前模拟的认识论弱点源于这样一个事实,即它们没有依赖任何独立的证据来证明温室气体在足够长的时间内对气候的影响。特别是,只要气候变化的最重要特征,即冰川-间冰期的转变和间冰期的不同持续时间,仍然没有得到解释,模型的有效性就不会得到证明。类似地,常数7 冰川消退后温度和二氧化碳减少之间的kyr时间滞后是另一个需要理解的重要特征。从这个角度来看,当前的气候辩论应该被视为地球科学进程中最新的重大争议,尽管它与之前的辩论有着明显的不同,其社会、环境、经济和政治影响最为多样。
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来源期刊
History of Geo- and Space Sciences
History of Geo- and Space Sciences GEOSCIENCES, MULTIDISCIPLINARY-HISTORY & PHILOSOPHY OF SCIENCE
CiteScore
1.50
自引率
33.30%
发文量
10
审稿时长
50 weeks
期刊介绍: The scope of History of Geo- and Space Sciences (HGSS) is to document historical facts and knowledge and to improve awareness of the history of geoscience. The knowledge of the development of geosciences and their experimental methods and theories in the past can improve our current understanding and may stimulate current research. It is encouraging for young scientists to read biographical material of historical figures in their research area. It is important as well to learn that history of science is an integrated part of the ongoing research in their research area. Another important aim of the journal is the association of historical retrospective and current research.
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