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Old World megadroughts and pluvials during the Common Era

机译:共同时期的旧世界大洪水和暴雨

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摘要

Climate model projections suggest widespread drying in the Mediterranean Basin and wetting in Fennoscandia in the coming decades largely as a consequence of greenhouse gas forcing of climate. To place these and other “Old World” climate projections into historical perspective based on more complete estimates of natural hydroclimatic variability, we have developed the “Old World Drought Atlas” (OWDA), a set of year-to-year maps of tree-ring reconstructed summer wetness and dryness over Europe and the Mediterranean Basin during the Common Era. The OWDA matches historical accounts of severe drought and wetness with a spatial completeness not previously available. In addition, megadroughts reconstructed over north-central Europe in the 11th and mid-15th centuries reinforce other evidence from North America and Asia that droughts were more severe, extensive, and prolonged over Northern Hemisphere land areas before the 20th century, with an inadequate understanding of their causes. The OWDA provides new data to determine the causes of Old World drought and wetness and attribute past climate variability to forced and/or internal variability.
机译:气候模型预测表明,在未来几十年中,由于温室气体强迫气候的影响,地中海盆地将普遍出现干旱,而芬诺斯坎迪亚州则变湿。为了根据对自然水文气候变异性的更完整估算,将这些和其他“旧世界”气候预测放到历史角度,我们开发了“旧世界干旱地图集”(OWDA),这是一组按年绘制的树状图,环重建了共同时期欧洲和地中海盆地的夏季干湿状况。 OWDA将严重干旱和潮湿的历史记录与以前没有的空间完整性进行了匹配。此外,在11世纪和15世纪中叶在欧洲中北部重建的大旱灾,进一步强化了来自北美和亚洲的其他证据,表明在20世纪之前,北半球陆地地区的干旱更加严重,范围广泛且持续时间较长,人们对此了解不足原因。 OWDA提供了新的数据来确定旧世界干旱和潮湿的原因,并将过去的气候变化归因于强迫和/或内部变化。

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