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A Method for Palaeoclimatic Reconstruction in Palynology Based on Multivariate Time-Series Analysis

机译:基于多元时间序列分析的孢粉学古气候重建方法

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摘要

A method based on multiple regression, canonical correlation analysis and the Kalman filter is developed with a view to producing a reliable reconstruction of climate from pollen spectra. The study region is the southern France, where traditional analytical techniques are unsatisfactory due to the heavy influence of human activity and the existence of a complex climate. The first stage of the proposed method is the same as the standard techniques in which a spatial network of 36 sites with recent pollen and climate data were analyzed by regression techniques. But since the recent data are frequently subjected to disturbance by such factors as human activity or the particularities of the local vegetations, a second, independent analytical stage was added, in which pairs of fossil sites were compared using ancient data exclusively. In this way a model of the climatic forcing can be obtained, with the above-mentioned factors left out of account. The reconstructions obtained from the first two stages were then compared in the third stage of the method, and the result is a corrected reconstruction, from which it appears that at 14 000 BP annual temperature was 9oC cooler than present, with a 4°C increase between 13 500 and 11 500 BP followed by a 2oC cooling at 10 500 BP. The Holocene temperature maximum occurred between 8000 and 6000 BP. when the temperature was 1°C warmer than present.
机译:提出了一种基于多元回归,典型相关分析和卡尔曼滤波的方法,以期从花粉光谱中得出可靠的气候重建结果。研究区域位于法国南部,由于人类活动的严重影响和复杂气候的存在,传统的分析技术无法令人满意。所提出方法的第一阶段与标准技术相同,在标准技术中,通过回归技术分析了包含最近花粉和气候数据的36个站点的空间网络。但是,由于最近的数据经常受到人类活动或当地植被的特殊性等因素的干扰,因此增加了第二个独立的分析阶段,其中仅使用古代数据比较了成对的化石遗址。这样,可以获得气候强迫模型,而无需考虑上述因素。然后将从前两个阶段获得的重建结果在方法的第三阶段中进行比较,结果是校正后的重建结果,从中可以看出,在14000 BP时,年温度比现在低9oC,升高了4°C。温度介于13500和11500 BP之间,然后在10500 BP下进行2oC冷却。全新世温度最高发生在8000和6000 BP之间。当温度比现在高1°C时。

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  • 作者

    Guiot Joël;

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  • 年度 1985
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  • 原文格式 PDF
  • 正文语种 en
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