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Shoreline variability of an urban beach fronted by a beachrock reef from video imagery

机译:视频影像中海滩岩石礁面向的城市海滩的海岸线变化

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摘要

This contribution presents the results of a study on the shoreline variability of a natural perched urban beach (Ammoudara, N. Crete, Greece). Shoreline variability was monitored in high spatio-temporal resolution using time series of coastal video images and a novel, fully automated 2-D shoreline detection algorithm. Ten-month video monitoring showed that cross-shore shoreline change was, in some areas, up to 8 m with adjacent sections of the shoreline showing contrasting patterns of beach loss or gain. Variability increased in spring/early summer and stabilized until the end of the summer when partial beach recovery commenced. Correlation of the patterns of beach change with wave forcing (as recorded at an offshore wave buoy) is not straightforward; the only discernible association was that particularly energetic waves from the northern sector can trigger changes in the patterns of shoreline variability and that increased variability might be sustained by increases in offshore wave steepness. It was also found that the fronting beachrock reef exerts significant geological control on beach hydrodynamics. Hydrodynamic modelling and observations during an energetic event showed that the reef can filter wave energy in a highly differential manner, depending on its local architecture. In some areas, the reef allows only low-energy waves to impinge on the shoreline, whereas elsewhere penetration of higher waves is facilitated by the low elevation and limited width of the reef or by the presence of an inlet. Wave/reef interaction can also generate complex circulation patterns, including rip currents that appeared to be also constrained by the reef architecture.
机译:这一贡献提出了对自然栖息的城市海滩(希腊,克里特岛,Ammoudara)海岸线变化的研究结果。使用沿海视频图像的时间序列和新颖的全自动二维海岸线检测算法,可以在高时空分辨率下监控海岸线变化。历时10个月的视频监控显示,在某些地区,跨岸海岸线的变化最大为8 m,而海岸线的相邻部分则显示出不同的海滩损失或增加模式。春季/初夏的变异性增加,直到夏末开始部分海滩恢复时才稳定下来。海滩变化模式与波浪强迫的相关性(如在海上波浪浮标上记录的)并不容易。唯一可辨别的关联是,来自北部地区的特别是高能波会触发海岸线变化形式的变化,而变化性的增加可能会随着近海波陡度的增加而持续。还发现,前沿滩石礁对滩水动力具有重要的地质控制作用。高能事件期间的流体动力学建模和观察表明,礁石可以根据其局部结构以高度差分的方式过滤波浪能。在某些地区,礁石仅允许低能波撞击海岸线,而在其他地方,礁石的高度低,宽度有限或存在入口,有助于较高波的穿透。波浪/礁石相互作用还可以产生复杂的循环模式,包括似乎也受到礁石结构限制的裂隙电流。

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