利用无人机系统安装的多波束激光雷达估算非破碎波中的定向波谱特性

Falk Feddersen, Olavo B. Marques, James H. MacMahan, Robert L. Grenzeback
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摘要

波谱和方向力矩测量具有科学和工程学意义,通常使用波浪浮标进行估算。最近,安装在固定地点和无人驾驶飞机系统(UAS)上的激光雷达估算了冲浪区的波谱。然而,由于回波数较低,激光雷达还没有测量过冲浪区海面的近岸波浪统计量,也没有测量过近岸方向力矩。我们使用安装在以汽油为动力的无人机系统上的多波束扫描激光雷达,通过 11 分钟的悬停,估算了水深≈ 10 米的内陆架的波谱、波坡谱和方向矩,并与同位波浪浮标进行了比较。半径 R 不同的圆形采样区域内的激光雷达回波与平面和二维抛物线拟合,提供海面和斜坡时间序列。当 R ≥ 0.8 米时,可以稳健地估算出海面波谱(0.04-0.4 赫兹)。大 R 在涌浪波段效果好,小 R 在较高频率效果好,与波浪浮标推断的斜率谱很一致。根据波谱、坡谱和横谱估算出的方向傅里叶系数与海涌波段的波浪浮标进行了比较。较大的 R 和二维抛物线拟合与波浪浮标的比较结果更好。在 R = 2.4 米和二维抛物线拟合条件下,在波浪浮标的不确定性范围内,平均波浪角和方向展宽(方向傅里叶系数的函数)得到了很好的再现。无人机系统激光雷达衍生结果的内部一致性及其与 Spotter 波浪浮标的良好对比证明了该工具在估算波浪统计数据方面的有效性。
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Estimating Directional Wave Spectra Properties in Non-Breaking Waves from a UAS-Mounted Multi-beam Lidar
Wave spectra and directional moment measurements are of scientific and engineering interest and are routinely estimated with wave buoys. Recently, both fixed-location and Uncrewed Aircraft System (UAS)-mounted lidar have estimated surfzone wave spectra. However, nearshore wave statistics seaward of the surfzone have not been measured with lidar due to low return number and nearshore directional moments have not been measured at all. We use a multi-beam scanning lidar mounted on a gasoline-powered UAS to estimate wave spectra, wave slope spectra, and directional moments on the inner shelf in ≈ 10 m water depth from an 11-min hover and compare to a co-located wave buoy. Lidar returns within circular sampling regions with varying radius R are fit to a plane and a 2D parabola, providing sea-surface and slope timeseries. Wave spectra across the sea-swell (0.04–0.4 Hz) are robustly estimated for R ≥ 0.8 m. Estimating slope spectra is more challenging. Large R works well in the swell band and smaller R work well at higher frequencies, in good agreement with a wave buoy inferred slope spectrum. Directional Fourier coefficients, estimated from wave and slope spectra and cross-spectra, are compared to a wave buoy in the sea-swell band. Larger R and the 2D parabola-fit yield better comparison to the wave buoy. Mean wave angles and directional spreads, functions of the directional Fourier coefficients, are well reproduced at R = 2.4 m and the 2D parabola-fit, within the uncertainties of the wave buoy. The internal consistency of the UAS-lidar-derived results and their good comparison to the Spotter wave buoy demonstrate the effectiveness of this tool for estimating wave statistics.
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