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Field Measurements of Wave Characteristics on a Near-Horizontal Shore Platform, Mahia Peninsula, North Island, New Zealand

机译:新西兰北岛马希亚半岛近水平岸平台波浪特征的现场测量

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Waves are an important process responsible for the initiation and subsequent development of intertidal shore platforms. However, few field studies to date have described wave processes on shore platforms. A field experiment was conducted using an across-shore array of wave gauges, including a directional sensor, on a near-horizontal platform at Mahia Peninsula, North Island, New Zealand. Results show that the platform is very efficient in filtering wave energy at gravity wave frequencies (>0.05 Hz), with 40-80% reduction in wave height measured across the 140 m wide platform. By contrast, infragravity waves are present on the platform and increase in magnitude towards the cliff toe. Directional wave analysis indicates that wave reflection is mainly restricted to infragravity wave frequencies, demonstrating the differences in gravity and infragravity wave behaviour on the platform studied. Results indicate that, under fair weather conditions, the role of waves as an agent of cliff toe erosion is likely to be limited at present, although they are probably important for removing sediments accumulated at the cliff toe. The observed increase in infragravity wave energy towards the cliff toe implies that these long-period waves may be important geomorphic agents on shore platforms.
机译:波浪是一个重要的过程,它负责潮间带岸台的启动和后续发展。但是,迄今为止,很少有现场研究描述海岸平台上的波浪过程。在新西兰北岛马希亚半岛的近水平平台上,使用包括定向传感器在内的一系列波导管进行了现场实验。结果表明,该平台在过滤重力波频率(> 0.05 Hz)下的波能方面非常有效,在140 m宽的平台上测得的波高降低了40-80%。相比之下,平台上存在次重力波,并向悬崖脚趾增大。定向波分析表明,波反射主要限于次重力波频率,这说明了所研究平台上重力和次重力波行为的差异。结果表明,在晴朗的天气条件下,波浪对悬崖脚趾侵蚀的作用目前可能受到限制,尽管它们对于清除悬崖脚趾上堆积的沉积物可能很重要。观察到的朝向悬崖脚趾的重力波能量的增加表明,这些长周期波可能是海岸平台上的重要地貌动因。

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