Recalculation of minimum wave heights from coastal boulder deposits in the Bristol Channel and Severn Estuary, UK: implications for understanding the high-magnitude flood event of AD 1607

IF 1.2 4区 地球科学 Q2 GEOLOGY
S. Haslett, Bernardine R. Wong
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引用次数: 0

Abstract

A high-magnitude coastal flood event catastrophically affected the macrotidal Bristol Channel and Severn Estuary in southwest Great Britain, United Kingdom, on 30th January 1607 causing an estimated 2000 fatalities. Historical and physical evidence has provided a basis for the development of a theory that the flood may have been due to a tsunami rather than a storm. Previous studies have collected field data to test this hypothesis including a dataset of 136 wave-transported boulder clasts that was utilised to estimate minimum wave heights through hydrodynamic equations in 2007, but the dataset has hitherto remained unpublished in full. Since 2007 these equations have undergone refinement and for this paper minimum wave heights were recalculated from boulder measurements using revised hydrodynamic equations and presents the complete dataset for the first time. A recent study claiming that such equations are flawed is considered premature, given ongoing refinements to the equations. The results of the present study indicate that a tsunami 4.2 m high can explain the dislodgement of all boulders measured, equivalent to a storm wave height of 16.9 m, which is considerably greater than observed storm wave heights in the region. An up-channel increase in minimum wave height is also suggested by these data, generally corroborating the 2007 study, which may be due to wave amplification caused by the overall funnel-shape of the embayment. The areas worst affected by the 1607 flood are located in the coastal lowlands of the inner Bristol Channel and Severn Estuary, coinciding with the highest minimum estimated wave heights.
英国布里斯托尔海峡和塞文河口海岸巨石沉积物最小波高的重新计算:对理解公元1607年高震级洪水事件的意义
1607年1月30日,英国西南部布里斯托尔海峡和塞文河口发生了一次高震级的沿海洪水事件,造成约2000人死亡。历史和物理证据为一种理论的发展提供了基础,即洪水可能是由海啸而不是风暴引起的。之前的研究已经收集了现场数据来验证这一假设,其中包括一个由136个波浪传播的巨石碎屑组成的数据集,该数据集用于通过2007年的流体动力学方程估计最小波高,但该数据集迄今为止尚未完整发表。自2007年以来,这些方程经过了改进,本文使用修订的水动力方程从巨石测量中重新计算了最小波高,并首次提供了完整的数据集。最近的一项研究声称这样的方程是有缺陷的,考虑到对方程的不断改进,这被认为是不成熟的。本研究结果表明,4.2 m高的海啸可以解释所有测量到的巨石的移动,相当于16.9 m的风暴波高,这比该地区观测到的风暴波高要高得多。这些数据还表明,通道上方的最小波高增加,总体上证实了2007年的研究,这可能是由于海湾的整体漏斗形状引起的波浪放大。受1607年洪水影响最严重的地区位于布里斯托尔海峡和塞文河口的沿海低地,与估计的最高最低浪高相吻合。
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来源期刊
Atlantic Geology
Atlantic Geology GEOLOGY-
CiteScore
2.10
自引率
18.80%
发文量
0
审稿时长
>12 weeks
期刊介绍: Atlantic Geology (originally Maritime Sediments, subsequently Maritime Sediments and Atlantic Geology) covers all aspects of the geology of the North Atlantic region. It publishes papers, notes, and discussions on original research and review papers, where appropriate to the regional geology.
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