大洪水
海洋学
地质学
海岸
全新世
自然地理学
合并(版本控制)
暴发洪水
气候学
环境科学
地理
考古
计算机科学
情报检索
作者
Sam J. Purkis,Steven N. Ward,Bolton Howes,Jake Longenecker,Morgan Chakraborty,Ákos Kálmán,Amy Clement,Arash Sharifi,Francesca Benzoni,Christopher R. Clarke,Mattie Rodrigue
出处
期刊:Science Advances
[American Association for the Advancement of Science]
日期:2025-02-21
卷期号:11 (8)
标识
DOI:10.1126/sciadv.adq3173
摘要
Intense rain can trigger flashfloods in Arabia. Torrential rains in 2024 sowed widespread chaos in the region. Sediment-loaded plumes discharged by flashfloods deposit onto the seabed. Burrowing animals disrupt these flood layers, erasing the paleorainfall record. Fortuitously, we discovered an anoxic deep-sea brine pool sited close enough to shore to chronicle floods, yet be otherwise undisturbed by animals. Cores retrieved from the pool delivered a 1600-year rainfall record. We merge these core-layer histories with modern rainfall statistics, satellite observations, and simulations to deliver a high-resolution quantitative Late Holocene hydroclimate record for Arabia. We find that the modern era is 2.5 times drier than the last 1.6 thousand years. The Little Ice Age stands out as particularly wet. That period experienced a fivefold increase in rainfall intensity compared to today. Though hyperarid now, the flood layers demonstrate that climate shifts can generate weather conditions unwitnessed in the modern era. Such long-range insight is crucial for framing uncertainties surrounding future hydroclimate forecasts.
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