Coastal Retreat on the Spanish Mediterranean Coast in a Climate Change Context: Effects of the Regulation of the Segura River at Its Mouth and the Coastal Sand Dune in Guardamar del Segura (Alicante, Spain)

Coasts Pub Date : 2024-02-02 DOI:10.3390/coasts4010005
Antonio Oliva, Jorge Olcina, A. Ollero
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Abstract

Coastal retreat processes are usually associated with many anthropogenic actions, such as the regulation of river basins, the construction of hydraulic storm defence works in coastal areas and the building of housing on the beach. To all of this, we should also add the increase in sea levels due to the effect of climate change. The chosen area of study corresponds to the coastal area of the municipality of Guardamar del Segura, belonging to the Segura River Basin. The methodology applied in this study comprised the gathering of historical information, the extraction of data using GIS, the compiling of data using official organisations and the analysis of all these data from a geographical perspective. The obtained results show the chronology of the regulation works in the Segura Basin and their relationship with the reduction and negative trend in average ordinary flows (1940–2023) and the extraordinary, swelled flows recorded in the period 1994–2023. Furthermore, the coastlines from 1923 to 2023 were mapped, enabling us to determine the evolution of the coastline retreat processes experienced in the dune ridge of Guardamar del Segura and the increase in the frequency of impacts due to storms on Babilonia Beach. Finally, data on wind, waves and marine currents recorded at a gauging station were incorporated, enabling us to understand their impact on this coastal sector. The results obtained are discussed, and they indicate the need to incorporate data on sediment into the study in order to complete it. The conclusions reveal the existence of a relationship between all these anthropogenic elements in the beach erosion processes experienced in the village of Guardamar del Segura.
气候变化背景下西班牙地中海海岸的海岸退缩:塞古拉河河口和瓜尔达马-德尔塞古拉(西班牙阿利坎特)沿海沙丘调节的影响
海岸后退过程通常与许多人为活动有关,如河流流域的治理、在沿海地区修建水利防 洪工程以及在海滩上建造房屋等。除此以外,我们还应该考虑到气候变化导致的海平面上升。所选择的研究区域是瓜尔达马-德尔塞古拉市的沿海地区,属于塞古拉河流域。本研究采用的方法包括收集历史信息、利用地理信息系统提取数据、利用官方组织汇编数据以及从地理角度分析所有这些数据。研究结果表明了塞古拉流域治理工程的时间顺序,以及这些工程与平均普通流量(1940-2023 年)减少和负增长趋势以及 1994-2023 年期间记录的异常膨胀流量之间的关系。此外,我们还绘制了 1923 年至 2023 年的海岸线图,从而确定了瓜尔达马-德尔塞古拉沙丘山脊海岸线后退过程的演变,以及巴比隆尼亚海滩受风暴影响频率的增加。最后,还纳入了测量站记录的风、波浪和洋流数据,使我们能够了解它们对这一沿海地区的影响。对所获得的结果进行了讨论,这些结果表明有必要将有关沉积物的数据纳入研究,以便完 成这项研究。结论显示,在瓜尔达马尔特塞古拉村经历的海滩侵蚀过程中,所有这些人为因素之间都存在关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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