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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Observations of coastal cliff base waves, sand levels, and cliff top shaking
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Observations of coastal cliff base waves, sand levels, and cliff top shaking

机译:观察沿海悬崖基波,沙水平和悬崖顶震动

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摘要

Concurrent observations of waves at the base of a southern California coastal cliff and seismic cliff motion were used to explore wave-cliff interaction and test proxies for wave forcing on coastal cliffs. Time series of waves and sand levels at the cliff base were extracted from pressure sensor observations programmatically and used to compute various wave impact metrics (e.g. significant cliff base wave height). Wave-cliff interaction was controlled by tide, incident waves, and beach sand levels, and varied from low tides with no wave-cliff impacts, to high tides with continuous wave-cliff interaction. Observed cliff base wave heights differed from standard Normal and Rayleigh distributions. Cliff base wave spectra levels were elevated at sea swell and infragravity frequencies. Coastal cliff top response to wave impacts was characterized using microseismic shaking in a frequency band (20-45Hz) sensitive to wave breaking and cliff impacts. Response in the 20-45Hz band was well correlated with wave-cliff impact metrics including cliff base significant wave height and hourly maximum water depth at the cliff base (r(2) = 0.75). With site-specific calibration relating wave impacts and shaking, and acceptable anthropogenic (traffic) noise levels, cliff top seismic observations are a viable proxy for cliff base wave conditions. The methods presented here are applicable to other coastal settings and can provide coastal managers with real time coastal conditions. Copyright (C) 2016 John Wiley & Sons, Ltd.
机译:在加利福尼亚南部沿海悬崖底部的海浪和地震悬崖运动的并发观测资料被用来探索海浪-悬崖相互作用,并测试在沿海悬崖上强迫海浪的代理。以编程方式从压力传感器的观测值中提取出悬崖底部的波浪和沙级的时间序列,并用于计算各种波浪冲击指标(例如重要的悬崖基础波浪高度)。波浪峭壁的相互作用受潮汐,入射波和海滩沙水平的控制,范围从无波浪峭壁影响的低潮汐到具有连续波浪峭壁相互作用的高潮。观测到的悬崖基波高度不同于标准正态分布和瑞利分布。悬崖基波频谱水平在海浪和次重力频率下升高。沿海悬崖顶部对波浪冲击的响应的特征是在对波浪破碎和悬崖冲击敏感的频带(20-45Hz)中使用微地震波来表征。在20-45Hz频段内的响应与波浪悬崖的影响指标具有很好的相关性,包括悬崖基础的显着波高和每小时在悬崖基础上的最大水深(r(2)= 0.75)。通过与波影响和晃动相关的特定于现场的校准以及可接受的人为(交通)噪声水平,悬崖顶地震观测可以替代悬崖基波条件。此处介绍的方法适用于其他沿海环境,并且可以为沿海管理人员提供实时的沿海条件。版权所有(C)2016 John Wiley&Sons,Ltd.

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