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近千年来东地中海地区气候与社会复原力建模

Modelling Climate and Societal Resilience in the Eastern Mediterranean in the Last Millennium.

作者信息

Xoplaki Elena, Luterbacher Jürg, Wagner Sebastian, Zorita Eduardo, Fleitmann Dominik, Preiser-Kapeller Johannes, Sargent Abigail M, White Sam, Toreti Andrea, Haldon John F, Mordechai Lee, Bozkurt Deniz, Akçer-Ön Sena, Izdebski Adam

机构信息

1Climatology, Climate Dynamics and Climate Change, Department of Geography, Justus-Liebig-University Giessen, Giessen, Germany.

2Centre of International Development and Environmental Research, Justus-Liebig-University Giessen, Giessen, Germany.

出版信息

Hum Ecol Interdiscip J. 2018;46(3):363-379. doi: 10.1007/s10745-018-9995-9. Epub 2018 Apr 19.

Abstract

This article analyses high-quality hydroclimate proxy records and spatial reconstructions from the Central and Eastern Mediterranean and compares them with two Earth System Model simulations (CCSM4, MPI-ESM-P) for the Crusader period in the Levant (1095-1290 CE), the Mamluk regime in Transjordan (1260-1516 CE) and the Ottoman crisis and Celâlî Rebellion (1580-1610 CE). During the three time intervals, environmental and climatic stress tested the resilience of complex societies. We find that the multidecadal precipitation and drought variations in the Central and Eastern Mediterranean cannot be explained by external forcings (solar variations, tropical volcanism); rather they were driven by internal climate dynamics. Our research emphasises the challenges, opportunities and limitations of linking proxy records, palaeoreconstructions and model simulations to better understand how climate can affect human history.

摘要

本文分析了地中海中部和东部地区高质量的水文气候代用记录和空间重建数据,并将其与两个地球系统模型模拟结果(CCSM4、MPI-ESM-P)进行比较,这两个模拟针对的是黎凡特地区的十字军时期(公元1095 - 1290年)、约旦的马穆鲁克政权时期(公元1260 - 1516年)以及奥斯曼危机和切莱比叛乱时期(公元1580 - 1610年)。在这三个时间段内,环境和气候压力考验了复杂社会的复原力。我们发现,地中海中部和东部地区多年代际的降水和干旱变化无法用外部强迫因素(太阳活动变化、热带火山活动)来解释;相反,它们是由内部气候动态驱动的。我们的研究强调了将代用记录、古重建和模型模拟联系起来以更好地理解气候如何影响人类历史所面临的挑战、机遇和局限性。

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