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利用来自土耳其西部的树木年轮数据改进对 5-6 月降水的重建及其与火山爆发的联系。

An improved reconstruction of May-June precipitation using tree-ring data from western Turkey and its links to volcanic eruptions.

机构信息

Forest Botany Department, Faculty of Forestry, Istanbul University, 34473, Bahçeköy, Istanbul, Turkey.

出版信息

Int J Biometeorol. 2013 Sep;57(5):691-701. doi: 10.1007/s00484-012-0595-x. Epub 2012 Sep 27.

Abstract

We developed a high quality reconstruction of May-June precipitation for the interior region of southwestern Turkey using regional tree-ring data calibrated with meteorological data from Burdur. In this study, three new climate sensitive black pine chronologies were built. In addition to new chronologies, four previously published black pine chronologies were used for the reconstruction. Two separate reconstructions were developed. The first reconstruction used all site chronologies over the common interval AD 1813-2004. The second reconstruction used four of the chronologies with a common interval AD 1692-2004. R² values of the reconstructions were 0.64 and 0.51 with RE values of 0.63 and 0.51, respectively. During the period AD 1692-1938, 41 dry and 48 wet events were found. Very dry years occurred in AD 1725, 1814, 1851, 1887, 1916, and 1923, while very wet years occurred in AD 1736, 1780, 1788, 1803, and 1892. The longest dry period was 16 years long between 1860 and 1875. We then explored relationships between the reconstructed rainfall patterns and major volcanic eruptions, and discovered that wetter than normal years occurred during or immediately after the years with the largest volcanic eruptions.

摘要

我们利用布尔杜尔的气象数据对区域树木年轮数据进行校准,为土耳其西南部内陆地区的 5-6 月降水重建了高质量的结果。在这项研究中,我们建立了三个新的气候敏感的黑松年表。除了新的年表外,我们还使用了之前发表的四个黑松年表进行重建。我们开发了两个独立的重建。第一个重建使用了共同时间段内(公元 1813-2004 年)的所有站点年表。第二个重建使用了共同时间段内(公元 1692-2004 年)的四个年表。重建的 R²值分别为 0.64 和 0.51,RE 值分别为 0.63 和 0.51。在公元 1692-1938 年期间,发现了 41 个干旱事件和 48 个湿润事件。非常干旱的年份发生在公元 1725 年、1814 年、1851 年、1887 年、1916 年和 1923 年,而非常湿润的年份发生在公元 1736 年、1780 年、1788 年、1803 年和 1892 年。最长的干旱期是 1860 年至 1875 年之间的 16 年。然后,我们探索了重建降雨模式与主要火山爆发之间的关系,发现较湿润的年份出现在最大的火山爆发年份或之后的年份。

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