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Shoreline variations and coastal dynamics: A space-time data analysis of the Jonian littoral, Italy

机译:海岸线变化和海岸动力学:意大利乔尼(Jonian)滨海地区的时空数据分析

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Morphological variations of coastlines are caused by several key processes that are influenced by climate conditions, sea level variations, wave energy, tectonics and human-induced phenomena. These processes affect the dynamics of catchment basins and the coastal environment. Since the second half of the 20th century, the Jonian coast of the Basilicata Region (Italy) has witnessed a widespread retreating phenomenon, predominantly due to anthropogenic causes affecting transport processes along the riverbeds and causing reductions in the sediment supply to the coast. The disturbance in the balance between sediment transport carried out by the sea and the sediment supply performed by rivers has led to a deficit in the sediment budget. To understand the morphological dynamics of the littoral environment and quantify the amount of coastal erosion, an analysis of coastline change has been carried out using various data sources: historical cartography, aerial photographs and GPS surveys. Between 1870 and 1954, the 32-km-long Jonian littoral under examination showed an accretion trend, while the loss in beach surface steadily increased between 1954 and 2005. The average change in beach surface has been calculated as about +55,000 m~2/yr (accretion) between 1870 and 1954 and -16,500 m~2/yr (erosion) between 1954 and 2005. Overall, 640,000 m~2 of sandy beaches were lost along the entire Jonian coast of the Basilicata Region between 1954 and 2005. Comparing the shoreline between 1870 and 1954, the average net shoreline movement (NSM) is +110 m vs. -30 m between 1954 and 2005. This analysis approach has proven to be effective in quantifying the erosion phenomenon and its effects, despite the lack of homogeneous data series and the variety of spatial and temporal scales over which coastal evolution occurs. The study represents an important step in understanding coastal dynamics in this region. As coastal areas are being affected by an increasing number of population and socio-economic activities, identification of shoreline changes and forecasts of coastline evolution represent key information for coastal scientists, engineers, decision makers and stakeholders for both the management of and development of future plans for coastal environments and for reducing exposure risk to coastal erosion.
机译:海岸线的形态变化是由几个关键过程引起的,这些关键过程受气候条件,海平面变化,波能,构造和人为现象的影响。这些过程影响集水盆地和沿海环境的动态。自20世纪下半叶以来,巴西利卡塔地区(意大利)的乔尼海岸发生了广泛的撤退现象,主要是由于人为原因影响了沿河床的运输过程,并减少了向海岸的沉积物供应。海上进行的泥沙输送与河流进行的泥沙供应之间的平衡失衡导致泥沙预算短缺。为了了解沿海环境的形态动态并量化海岸侵蚀的数量,已使用各种数据源对海岸线变化进行了分析:历史制图,航拍照片和GPS调查。在1870年和1954年之间,受检查的32公里长的Jonian沿海地区呈增生趋势,而在1954年至2005年之间,海滩表面的损失稳定增加。据计算,海滩表面的平均变化约为+55,000 m〜2 / 1870年至1954年之间的年(增生)和1954年至2005年之间的-16,500 m〜2 /年(侵蚀)。1954年至2005年之间,整个巴西利卡塔地区约拿海岸的沙滩损失了640,000 m〜2。在1870年至1954年之间的海岸线上,平均净海岸线运动(NSM)为+110 m,而1954年至2005年之间为-30 m。尽管缺乏分析方法,但该分析方法已被证明可有效地量化侵蚀现象及其影响。同类数据序列以及发生沿海演变的各种时空尺度。这项研究代表了了解该地区沿海动态的重要一步。由于沿海地区正受到越来越多的人口和社会经济活动的影响,海岸线变化的识别和海岸线演变的预测为沿海科学家,工程师,决策者和利益相关者提供了管理和制定未来计划的关键信息用于沿海环境和减少遭受海岸侵蚀的风险。

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