Breaks, Trends and the Attribution of Climate Change: A Time-Series Analysis

F. Estrada, Pierre Perron
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引用次数: 9

Abstract

Climate change detection and attribution have been the subject of intense research and debate over at least four decades. However, direct attribution of climate change to anthropogenic activities using observed climate and forcing variables through statistical methods has remained elusive, partly caused by the difficulties for correctly identifying the time-series properties of these variables and by the limited availability of methods for relating nonstationary variables. This paper provides strong evidence concerning the direct attribution of observed climate change to anthropogenic greenhouse gases emissions by first investigating the univariate time-series properties of observed global and hemispheric temperatures and forcing variables and then by proposing statistically adequate multivariate models. The results show that there is a clear anthropogenic fingerprint on both global and hemispheric temperatures. The signal of the well-mixed GHG forcing in all temperature series is very clear and accounts for most of their secular movement since the beginning of observations. Both temperature and forcing variables are characterized by piecewise linear trends with abrupt changes in their slopes estimated to occur at different dates. Nevertheless, their long-term movements are so closely related that the observed temperature and forcing trends cancel out. The warming experimented during the last century was mainly due to the increase in GHG which was partially offset by the effect of tropospheric aerosols. Other forcing sources, such as solar, are shown to only contribute to (shorter-term) variations around the GHG forcing trend.
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气候变化的中断、趋势和归因:一个时间序列分析
气候变化的探测和归因是近四十年来激烈研究和争论的主题。然而,通过统计方法利用观测到的气候和强迫变量将气候变化直接归因于人为活动仍然难以捉摸,部分原因是难以正确识别这些变量的时间序列特性,以及用于关联非平稳变量的方法的可用性有限。本文首先研究了观测到的全球和半球温度和强迫变量的单变量时间序列特性,然后提出了统计上适当的多变量模型,为观测到的气候变化直接归因于人为温室气体排放提供了强有力的证据。结果表明,人类活动对全球和半球温度都有明显的影响。所有温度序列中混合良好的温室气体强迫信号非常清晰,并解释了自观测开始以来它们的大部分长期运动。温度和强迫变量都具有分段线性趋势的特征,其斜率在不同日期估计会发生突变。然而,它们的长期运动是如此密切相关,以至于观测到的温度和强迫趋势相互抵消。在上个世纪试验的变暖主要是由于温室气体的增加,而对流层气溶胶的作用部分抵消了温室气体的增加。其他强迫源,如太阳,仅对温室气体强迫趋势周围的(短期)变化有所贡献。
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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