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High-magnitude flooding across Britain since AD 1750

机译:自公元1750年以来,英国发生了大洪水

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The last decade has witnessed severe flooding across much of the globe, but have these floods really been exceptional? Globally, relatively few instrumental river flow series extend beyond 50?years, with short records presenting significant challenges in determining flood risk from high-magnitude floods. A perceived increase in extreme floods in recent years has decreased public confidence in conventional flood risk estimates; the results affect society (insurance costs), individuals (personal vulnerability) and companies (e.g.?water resource managers). Here, we show how historical records from Britain have improved understanding of high-magnitude floods, by examining past spatial and temporal variability. The findings identify that whilst recent floods are notable, several comparable periods of increased flooding are identifiable historically, with periods of greater frequency (flood-rich periods). Statistically significant relationships between the British flood index, the Atlantic Meridional Oscillation and the North Atlantic Oscillation Index are identified. The use of historical records identifies that the largest floods often transcend single catchments affecting regions and that the current flood-rich period is not unprecedented.
机译:过去十年见证了全球大部分地区的严重洪灾,但是这些洪灾真的有例外吗?在全球范围内,相对较少的工具性河流径流序列能延续到50年以上,而短记录对确定高强度洪水的洪水风险提出了重大挑战。近年来,人们意识到极端洪水的增加,降低了公众对常规洪水风险估算的信心;结果会影响社会(保险成本),个人(个人脆弱性)和公司(例如水资源管理者)。在这里,我们展示了英国的历史记录如何通过检查过去的时空变化来增进对高强度洪水的理解。调查结果表明,尽管最近的洪灾很明显,但历史上可以确定几个可比的洪灾增加时期,其发生频率较高的时期(富洪时期)。确定了英国洪水指数,大西洋子午涛动和北大西洋涛动指数之间的统计显着性关系。历史记录的使用表明,最大的洪灾往往超过影响地区的单个流域,而当前的洪灾丰富时期并非前所未有。

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