首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Drifter observations of the effects of shoals and tidal-currents on wave evolution in San Francisco Bight
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Drifter observations of the effects of shoals and tidal-currents on wave evolution in San Francisco Bight

机译:关于旧金山湾中浅滩和潮流对波浪演化影响的漂流观测

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Detailed observations of wave evolution and wave-current interaction in tidal inlets and river mouths are practically non-existent. This is in part due to the practical difficulty of installing and maintaining fixed instruments in this harsh environment with large waves, strong currents, dynamic seabed morphology, and often busy ship traffic, but also due to the fact that it is difficult to resolve the spatial variability and evolution of the wave and current field from an array of point measurements. This work explores the use of newly developed small, free-drifting buoys to collect wave and current measurements in a coastal inlet. The instruments, referred to as wave-resolving drifters (or WRD), are small and lightweight enough so that they can be deployed and retrieved from small vessels, and relatively inexpensive so that large numbers can be used. The surface-following drifters resolve the three-dimensional wave orbital motion and surface current field by combining GPS and accelerometer measurements. We validate the WRD platform and its sensor package in open ocean conditions in Monterey Bay by comparing the WRD observations to observations made by a collocated 40 cm-diameter Datawell Waverider buoy. To study wave evolution in the San Francisco Bight, 30 WRDs are deployed near the San Francisco Bay entrance (Golden Gate) during peak ebb tide so that the drifters flow out of the bay, and into the incident wave field. Wave statistics are estimated through local ensemble averaging of drifter observations, and ensemble-averaged wave spectra are used to capture the wave evolution through the inlet area. Comparisons with numerical simulations of the simulating waves near shore (SWAN) model help identify the various processes acting on different frequency ranges of the wave field, and ray diagrams show the distinct effects of refraction by variable depth on the lower-frequency swells and refraction by currents on the higher-frequency wind waves. This combined analysis demonstrates the potential of using relatively inexpensive surface-following drifters to investigate surface dynamics in a complicated and energetic coastal inlet. Published by Elsevier Ltd.
机译:几乎没有潮汐进口和河口的波浪演化和波流相互作用的详细观测结果。这部分是由于在这种恶劣的环境中安装和维护固定仪器的实际困难,在这种恶劣的环境中存在着大波浪,强流,动态海床形态以及经常有繁忙的船舶通行的情况,而且还由于难以解决空间问题点测量阵列中波和电流场的变化和演变。这项工作探索了如何使用新开发的小型,可自由漂浮的浮标来收集沿海入口处的波浪和电流测量结果。这些仪器被称为消波漂移器(WRD),其体积小,重量轻,因此可以从小型容器中部署和取回,并且价格相对便宜,因此可以使用大量仪器。跟随地表的漂移器通过结合GPS和加速度计测量来解决三维波轨道运动和地表电流场。通过比较WRD观测值与并置的40厘米直径Datawell Waverider浮标的观测值,我们验证了蒙特雷湾公海条件下的WRD平台及其传感器组件。为了研究旧金山湾的波浪演化,在涨潮期间,在旧金山湾入口(金门)附近部署了30个WRD,以使漂流者从海湾流出并进入入射波场。通过对漂流观测资料进行局部平均,可以估算出海浪的统计数据,然后使用整体平均的波谱来捕获通过入口区域的海浪演变。与近岸模拟波(SWAN)模型的数值模拟进行比较有助于识别作用于波场不同频率范围的各种过程,并且射线图显示了可变深度的折射对低频膨胀的显着影响以及对波场的折射。高频风波上的电流。这项综合分析表明,使用相对便宜的地表流浪者研究复杂而充满活力的沿海进口地表动力学的潜力。由Elsevier Ltd.发布

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