近岸活力区沉积物动力学:声学遥感和模型验证

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
G. W. Wilson, P. Dickhudt, J. Aldrich
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引用次数: 0

摘要

使用 0.5、1.0 和 2.0 兆赫的多频声纳在破浪和非破浪情况下的近岸浅水环境中收集了声学反向散射数据。这些数据用于开发和测试一个声学反演模型,以测量破浪产生气泡时的悬浮沉积物浓度(SSC)。该模型利用气泡和沙粒声散射的频率依赖性对比,同时估算 SSC 和气泡空隙率。根据现场沉积物测量结果进行的验证表明,声学技术在破浪和非破浪情况下都能准确恢复沉积物浓度,这与仅在非破浪情况下表现良好的现有算法不同。最后,实验数据被用于验证现有的破浪条件下悬浮沉积物动力学理论,而现有的破浪条件下悬浮沉积物动力学数据集很少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sediment Dynamics in the Energetic Nearshore Zone: Acoustic Remote Sensing and Model Validation

Acoustic backscatter data were collected in the shallow nearshore environment under breaking and non-breaking waves, using a multi-frequency sonar at 0.5, 1.0, and 2.0 MHz. The data are used to develop and test an acoustic inverse model for measuring suspended sediment concentration (SSC) in the presence of bubbles generated by breaking waves. The model leverages the contrasting frequency dependence of acoustic scattering by bubbles and sand, to simultaneously estimate SSC and bubble void fraction. Validation against in situ sediment measurements shows the acoustic technique can recover sediment concentration with good accuracy in both breaking and non-breaking waves, unlike existing algorithms which only perform well in non-breaking waves. Finally, data from the experiment are used to validate existing theories for suspended sediment dynamics under breaking waves, for which few previous data sets exist.

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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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