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Sea level extremes in Marseille (NW Mediterranean) during 1885-2008

机译:1885-2008年间马赛(地中海西北地区)的极端海平面

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摘要

Sea level extremes and their temporal variability have been explored based on the hourly measurements at Marseille tide gauge for the period 1885-2008. A careful quality check has first been applied to the observations to ensure consistency of the record by eliminating outliers and datum shifts. Yearly percentiles have been used to investigate long-term trends of extremes revealing that secular variations in extremes are linked to mean sea level changes. The associated decadal changes show discrepancies between mean sea level trend and extreme fluctuations, due to the influence of the atmospheric forcing. A local regression model based on the generalized Pareto distribution has been applied to derive trends in return levels. The 50-years return levels reach values between 80 and 120. cm. The most significant changes in return levels are characterized by an increase since the 1970s.
机译:根据1885年至2008年期间马赛潮汐仪的小时测量值,探索了海平面的极端值及其随时间的变化。首先对观察结果进行了仔细的质量检查,以通过消除异常值和基准移动来确保记录的一致性。每年百分位被用于调查极端事件的长期趋势,揭示极端事件的长期变化与平均海平面变化有关。由于大气强迫的影响,相关的年代际变化显示出平均海平面趋势和极端波动之间的差异。基于广义帕累托分布的局部回归模型已应用于得出收益水平的趋势。 50年的回报水平达到80到120. cm之间的值。自1970年代以来,回报水平上最显着的变化是增长。

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