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首页> 外文期刊>Climate of the Past Discussions >Maximum growing season temperature in Western Europe: multi proxy reconstructions in Fontainebleau from 1596 to 2000
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Maximum growing season temperature in Western Europe: multi proxy reconstructions in Fontainebleau from 1596 to 2000

机译:西欧最高生长季节温度:1596年至2000年在枫丹白露的多代理重建

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In this study, we have combined a Burgundy grape harvest date record with new δ18O measurements conducted on timbers and living trees cellulose from Fontainebleau castle and forest. Our reconstruction is expected to provide a reference series for the variability of growing season temperature (from April to September) in Western Europe from 1596 to 2000. We have estimated an uncertainty of 0.55°C on individual growing season maximum temperature reconstructions. We are able to assess this uncertainty, which is not the case for many documentary sources (diaries etc.), and even not the case for early instrumental temperature data. We compare our data with a number of independent temperature estimates for Europe and the Northern Hemisphere. The comparison between our reconstruction and Manley mean growing season temperature data provides an independent control of the quality of CET data. We show that our reconstruction preserves more variance back in time, because it was not distorted/averaged by statistical/homogenisation methods. Further works will be conducted to compare the δ18O data from wood cellulose provided by transects of different tree species in Europe obtained within the EC ISONET project and the French ANR Program ESCARSEL, to analyse the spatial and temporal coherency between δ18O records. The decadal variability will be also compared with other precipitation δ18O records such as those obtained from benthic ostracods from deep peri-Alpine lakes or simulated by regional atmospheric models equipped with the modelling of water stable isotopes.
机译:在这项研究中,我们将勃艮第的葡萄收获日期记录与对枫丹白露城堡和森林的木材和活树纤维素进行的新的δ 18 O测量相结合。我们的重建预计将为1596至2000年西欧生长季节温度(4月至9月)的变化提供参考序列。我们估计,各个生长季节最高温度重建的不确定性为0.55°C。我们能够评估这种不确定性,对于许多文献资料(糖尿病等)而言,情况并非如此,对于早期仪器温度数据而言,情况甚至并非如此。我们将我们的数据与欧洲和北半球的许多独立温度估算值进行了比较。我们的重建数据和Manley平均生长季节温度数据之间的比较提供了对CET数据质量的独立控制。我们表明,我们的重建保留了更多的时差,因为它没有被统计/均质化方法扭曲/平均。还将进行进一步的工作,以比较EC ISONET项目和法国ANR计划ESCARSEL中从欧洲不同树种的样条提供的木材纤维素中的δ 18 O数据,以分析时空分布δ 18 O记录之间的相干性。年代际变率还将与其他降水δ 18 O记录进行比较,例如从深部近高山湖泊的底栖兽脚类动物获得的记录,或通过装有水稳定同位素模型的区域大气模型进行模拟。

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