Cook Edward R, Seager Richard, Kushnir Yochanan, Briffa Keith R, Büntgen Ulf, Frank David, Krusic Paul J, Tegel Willy, van der Schrier Gerard, Andreu-Hayles Laia, Baillie Mike, Baittinger Claudia, Bleicher Niels, Bonde Niels, Brown David, Carrer Marco, Cooper Richard, Čufar Katarina, Dittmar Christoph, Esper Jan, Griggs Carol, Gunnarson Björn, Günther Björn, Gutierrez Emilia, Haneca Kristof, Helama Samuli, Herzig Franz, Heussner Karl-Uwe, Hofmann Jutta, Janda Pavel, Kontic Raymond, Köse Nesibe, Kyncl Tomáš, Levanič Tom, Linderholm Hans, Manning Sturt, Melvin Thomas M, Miles Daniel, Neuwirth Burkhard, Nicolussi Kurt, Nola Paola, Panayotov Momchil, Popa Ionel, Rothe Andreas, Seftigen Kristina, Seim Andrea, Svarva Helene, Svoboda Miroslav, Thun Terje, Timonen Mauri, Touchan Ramzi, Trotsiuk Volodymyr, Trouet Valerie, Walder Felix, Ważny Tomasz, Wilson Rob, Zang Christian
Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.
Climatic Research Unit, University of East Anglia, Norwich NR4 7TJ, UK.
Sci Adv. 2015 Nov 6;1(10):e1500561. doi: 10.1126/sciadv.1500561. eCollection 2015 Nov.
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.
气候模型预测表明,在未来几十年里,地中海盆地将普遍干旱,而斯堪的纳维亚半岛将变得湿润,这主要是气候受到温室气体影响的结果。为了基于对自然水文气候变率更全面的估计,将这些以及其他“旧世界”气候预测置于历史背景中,我们编制了“旧世界干旱地图集”(OWDA),这是一套逐年的地图,展示了公元纪年期间欧洲和地中海盆地树木年轮重建的夏季湿润和干燥情况。OWDA将严重干旱和湿润的历史记录与以前无法获得的空间完整性相匹配。此外,在11世纪和15世纪中叶在欧洲中北部重建的大干旱强化了来自北美和亚洲的其他证据,即在20世纪之前,北半球陆地区域的干旱更加严重、广泛和持久,而人们对其成因了解不足。OWDA提供了新的数据,以确定旧世界干旱和湿润的成因,并将过去的气候变率归因于强迫和/或内部变率。