Two-and Three-Dimensional Laboratory Studies of Wave Breaking, Dissipation, Setup, and Runup on Reefs

暗礁 水槽 水深测量 地质学 波高 波浪变浅 折射 波浪水槽 浅滩化与学校教育 破碎波 波浪和浅水 消散 海底管道 边缘礁 反射(计算机编程) 流量(数学) 海洋学 波传播 机械 物理 光学 机械波 程序设计语言 纵波 热力学 计算机科学
作者
Ernest R. Smith,Tyler J. Hessner,Jane McKee Smith
标识
DOI:10.21236/ada586346
摘要

Physical model studies were performed at a 1-to-50 model to prototype scale in a three-dimensional (3-D) basin and a two-dimensional (2-D) flume to measure wave transformation, setup, and runup on a generalized reef to improve understanding of the processes.Incident wave and water level conditions encompassed a range of combinations representative of the geographical locations where reefs are present.Results from the 3-D experiment indicated higher frequency wave energy dissipated across the reef, whereas low frequency wave energy remained nearly constant.Three-dimensional patterns were observed on the reef, which was attributed to non-symmetrical bathymetry, wave-wave interactions, wave refraction, and reflection.Additional tests with an angled channel cut into the reef showed net offshore flow in the channel and near the reef centerline, where a net alongshore velocity also was measured.Wave heights were similar to the non-channel tests, but longer-period waves with higher incident heights generally showed greater heights in the shoaling region.A cross-section of the 3-D reef was duplicated and installed in a wave tank.The 2-D experiments were performed for similar wave and water level conditions as in the three-dimensional tests.Reef slopes of 1:2.5 and 1:5 were examined.Transformation results were similar to the 3-D tests except that a strong return flow was observed which increased breaker height.Reef roughness was varied for both the 2-D and 3-D tests, but had little effect on the waves, indicating that a rougher surface would be necessary to reduce wave height.

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