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Detection and attribution of flood trends in Mediterranean basins

机译:地中海盆地洪水趋势的检测与归因

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Floods have strong impacts in the Mediterranean region and there are concerns about a possible increase in their intensity due to climate change. In this study, a large database of 171 basins located in southern France with daily discharge data with a median record length of 45?years is considered to analyze flood trends and their drivers. In addition to discharge data, outputs of precipitation, temperature, evapotranspiration from the SAFRAN reanalysis and soil moisture computed with the ISBA land surface model are also analyzed. The evolution of land cover in these basins is analyzed using the CORINE database. The trends in floods above the 95th and 99th percentiles are detected by the Mann–Kendall test and quantile regression techniques. The results show that despite the increase in extreme precipitation reported by previous studies, there is no general tendency towards more severe floods. Only for a few basins is the intensity of the most extreme floods showing significant upward trends. On the contrary, most trends are towards fewer annual flood occurrences above both the 95th and 99th percentiles for the majority of basins. The decrease in soil moisture seems to be an important driver for these trends, since in most basins increased temperature and evapotranspiration associated with a precipitation decrease are leading to a reduction in soil moisture. These results imply that the observed increase in the vulnerability to these flood events in recent decades is mostly caused by human factors such as increased urbanization and population growth rather than climatic factors.
机译:洪水在地中海地区产生强烈影响,由于气候变化导致其强度的担忧令人担忧。在本研究中,位于法国南部的171个盆地的大型数据库,每日排放数据,中位数的记录长度为45岁,被认为是分析洪水趋势及其司机。除了放电数据外,还分析了沉淀,温度,蒸馏出来的Safran Reanalysis和土壤水分的蒸馏和用ISBA陆地表面模型计算的土壤水分。使用鲤鱼数据库分析这些盆地中的陆盖的演变。 Mann-Kendall测试和定量回归技术检测到95th和第99百分位上方的洪水趋势。结果表明,尽管先前研究报告的极端降水量增加,但对更严重的洪水没有一般倾向。只有几个盆地只是最极端洪水的强度,呈现出显着的上升趋势。相反,大多数趋势都是较少的年度洪水事件,以至于大多数盆地的95和第99百分位数。土壤水分的降低似乎是这些趋势的重要驾驶员,因为在大多数盆地中,与降水有关的温度和蒸散量降低导致土壤水分降低。这些结果意味着近几十年来观察到对这些洪水事件的脆弱性的增加主要是由人类因素引起的,例如城市化和人口增长而不是气候因素。

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