Mediating Climate Change

Sophie A. Day (Nee Nicholson-Cole)

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Mediating Climate Change

机译：调解气候变化

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Climate change: temporally complex, unseen and intangible, distant and decontextualised in the imagery that represents it, surrounded by discourses of (ir)rationality, uncertain yet urgent ... This book tackles a thorny issue, which over recent years has become more widely recognised and which permeates the science, politics and sociology of climate change: on an everyday basis, to the everyday person, how meaningful is it? Climate change may be a well-recognised phenomenon with a respected body of science, yet do people really care?

机译：气候变化：时间复杂，看不见，无形，遥远和去上下文化，在代表它的图像中，围绕着（非）理性，不确定但紧迫的论述...这本书解决了一个棘手的问题，近年来这个问题变得越来越广泛认识并渗透到气候变化的科学，政治和社会学中：在日常工作中，对于每天的人而言，这有多有意义？在受人尊敬的科学体系中，气候变化可能是公认的现象，但人们真的在乎吗？

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来源
《Journal of integrative Environmental Sciences》 |2013年第2期|143-144|共2页
作者
Sophie A. Day (Nee Nicholson-Cole);
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Tyndall Centre for Climate Change Research Faculty of Engineering and the Environment, Highfield Campus University of Southampton, Southampton SO 17 1BJ, UK;

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机译：气候变化和海豹生存：大象海豹Mirounga leonina幼崽生存的环境媒介变化证据
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

Mediating Climate Change

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