This paper presents a statistical analysis of structural changes in the Central England temperature series, one of the longest surface temperature records available. A changepoint analysis is performed to detect abrupt changes, which can be regarded as a preliminary step before further analysis is conducted to identify the causes of the changes (e.g., artificial, human-induced or natural variability). Regression models with structural breaks, including mean and trend shifts, are fitted to the series and compared via two commonly used multiple changepoint penalized likelihood criteria that balance model fit quality (as measured by likelihood) against parsimony considerations. Our changepoint model fits, with independent and short-memory errors, are also compared with a different class of models termed long-memory models that have been previously used by other authors to describe persistence features in temperature series. In the end, the optimal model is judged to be one containing a changepoint in the late 1980s, with a transition to an intensified warming regime. This timing and warming conclusion is consistent across changepoint models compared in this analysis. The variability of the series is not found to be significantly changing, and shift features are judged to be more plausible than either short- or long-memory autocorrelations. The final proposed model is one including trend-shifts (both intercept and slope parameters) with independent errors. The analysis serves as a walk-through tutorial of different changepoint techniques, illustrating what can be statistically inferred.
翻译:本文介绍了对中英格兰温度系列结构变化的统计分析,这是现有地表温度记录中最长的表层温度记录之一。为了检测突变的变化,对中英格兰温度系列的结构变化进行了变化点分析,在进一步分析确定变化的原因(例如人为变化、人为变化或自然变化)之前,可将这种变化视为初步步骤; 将结构间断(包括中值和趋势变化)的回归模型与该系列相匹配,并通过两个常用的多变点比较,使模型质量(按概率衡量)与偏差因素相匹配的可能性标准受到抑制。 我们的变点模型与独立和短镜头错误相匹配,也与其他作者以前用来描述温度序列中持久性特征的不同模型类长期模拟模型相比较。最后,认为最佳模型包含1980年代后期的变更点,包括向强化变暖制度过渡。这一时间和变暖结论与本次分析中的变化点模型是一致的。发现,该序列的变异性没有显著的变化,而且变异特征被认为比短期或短暂的模拟模型更可信,包括长期的推导式模型作为最后的推算。