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Changes in Storminess and surges in western France during the last century

机译:上个世纪法国西部的暴风雨和暴风雨变化

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摘要

French meteorological data provide some information on wind direction since 1890. Since 1951, wind speed and direction have been digitised every three hours in many stations. The Brest tide gauge has recorded hourly sea levels since 1860, thus enabling hourly surges to be calculated and studied. This set of data has been organised into a data base and analysed in order to recognize evolution and trends. Strong winds are increasing in frequency in the western part of Brittany and decreasing in Normandy and Pays de Loire. Surges associated with these winds do present a slight decreasing trend. A more precise analysis allows to distinguish between southerly winds, which are slightly decreasing, and strong winds from other directions, which display a more or less important increase in frequency. The analysis shows trends that may be linked to the global circulation pattern, and that result in a new spatial distribution of winds on western France.
机译:自1890年以来,法国气象数据就提供了一些有关风向的信息。自1951年以来,许多站点每三小时就将风速和风向数字化。自1860年以来,布雷斯特潮汐仪就记录了每小时的海平面,因此可以计算和研究每小时的潮汐。这组数据已组织到一个数据库中并进行了分析,以便识别演变和趋势。布列塔尼西部的强风频率增加,诺曼底和卢瓦尔河地区的强风频率减少。与这些风有关的浪潮确实呈现出轻微的下降趋势。更精确的分析可以区分稍有减少的南风和来自其他方向的强风,后者显示出或多或少重要的频率增加。分析表明趋势可能与全球环流模式有关,并导致法国西部风的新空间分布。

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