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Relationship between wave energy and coastal morphology in the central Algarve rocky coast (Galé to Olhos de Água)

机译:阿尔加威中部岩石海岸(加勒至奥卢什·德阿瓜)的波能与海岸形态之间的关系

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摘要

The coastal zones’ geomorphological evolution is the result of subaereal weathering andmarine abrasion. To quantify the role of the waves’ action as a geomorphic process particularlyon shore platforms sculpture is the main goal of the current work. For that purpose, a numericalmodeling for wave propagation (STWAVE) was used to determine differences on breakingwave characteristics along the study area. This program was used inside an operational toolbox(SMS 9.2) that allows data pre-processing from a GIS software (ArcGIS 9.2). The MATLABR2007a software was used to obtain significant wave heights and wave energy at the breakingposition along the study area, for each tested condition. The different coastal morphologies andmass movements were identified on the field and compared with the described evolution inliterature (Marques, 1997). Since the study area presents strong longshore variation inexposition to the waves and different wave energies, several sections were defined. It was thenpossible to analyze the frequency of occurrence of a given coastal morphology and the frequency of mass movements for each section and compare with longshore variations on waveenergy for both average and storm conditions.
机译:沿海地区的地貌演化是亚地缘性风化和海洋磨损的结果。量化波浪在地貌过程中的作用,尤其是在岸上平台雕塑上,是当前工作的主要目标。为此,使用了波传播的数值模型(STWAVE)来确定研究区域沿波特性的差异。该程序在可操作工具箱(SMS 9.2)中使用,该工具箱允许从GIS软件(ArcGIS 9.2)进行数据预处理。对于每种测试条件,使用MATLABR2007a软件获取沿研究区域的断裂位置处的显着波高和波能。在野外发现了不同的海岸形态和质量运动,并将其与描述的演化文学相比较(Marques,1997)。由于研究区域对波浪和不同的波浪能量表现出很强的近岸变化特征,因此定义了几个区域。然后有可能分析给定海岸形态的发生频率和每个断面的质量运动频率,并与平均和暴风雨条件下波浪能量的长岸变化进行比较。

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