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Long term January–March and May–August temperature reconstructions from tree-ring records from Bosnia and Herzegovina

机译:根据波斯尼亚和黑塞哥维那的树木年轮记录,对一月至三月和五月至八月进行长期温度重建

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We present the first spring and summer temperature reconstruction for the north-western part of the Balkan Peninsula. The reconstruction is based on tree-ring width measurements from 7 representative black pine (Pinus nigra Arnold) sites in Bosnia and Herzegovina (BiH). We found a significant, positive influence of above-average January–March temperatures on 4 sites (Blace, Peru?ica, ?ator, Konjuh) and a negative influence of above-average May–August temperatures and a positive relationship with an above-average sum of May–August precipitation on tree-ring width formation from 3 sites (Krivaja, Prusac, ?ipovo). A 31-yr running correlation between temperature and precipitation of the May–August period and tree-ring indices gave a stable relationship between 1901 and the 1960s, after which values of correlation coefficients decrease to the level of significance. A change in summer cyclones in the central part of the Adriatic Sea is presented as a possible cause of the divergence with the climate signal. In the period of calibration and verification of the linear model for the group of 3 sites (Krivaja, Prusac, ?ipovo), the best relationship was found between tree-ring indices and mean May–August temperatures of the current year. For the group of 4 sites (Blace, Peru?ica, ?ator, Konjuh), the relationship between tree-ring indices and mean January–March temperatures of the current year is the strongest. The developed models were used for reconstruction of May–August temperatures for BiH for the period 1701–1901 and January–March temperatures for the period 1685–1901. Using the method of percentiles (85th and 15th) we identified extreme hot/cool summers and warm/cold springs and compared them to available documentary historical sources and other reconstructions from the broader region.
机译:我们介绍了巴尔干半岛西北部的首次春季和夏季温度重建。重建是基于波斯尼亚和黑塞哥维那(BiH)的7个代表性黑松(Pinus nigra Arnold)站点的年轮宽度测量结果。我们发现1月至3月温度高于平均水平对4个地点(布莱斯,秘鲁,卡塔尔,肯特赫)有显着的积极影响,而5月至8月温度高于平均水平则有负面影响,而与5月至8月的高于3个地点(Krivaja,Prusac,?ipovo)5月至8月树轮宽度形成的平均降水量。 5月至8月期间温度和降水与树木年轮指数之间存在31年的连续相关性,从而在1901年至1960年代之间建立了稳定的关系,此后相关系数的值减小到显着水平。亚得里亚海中部夏季气旋的变化是气候信号发散的可能原因。在对三个地点(Krivaja,Prusac,?ipovo)的三个地点的线性模型进行的校准和验证期间,树木年轮指数与当年5月至8月的平均温度之间发现了最佳关系。对于4个站点的组(Blace,Peru?ica,?ator,Konjuh),树木年轮指数与当年1月至3月平均温度之间的关系最强。所开发的模型用于重建1701-1901年期间BiH的5月至8月的温度以及1685-1901年期间的1月至3月的温度。使用百分位方法(第85位和第15位),我们确定了炎热/凉爽的夏季和温暖/寒冷的春季,并将它们与可用的文献历史资料以及来自更广阔地区的其他重建资料进行了比较。

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