Wave heights obtained from sea surface and bottom measurements

Generally, the pressure response function of the most commonly used linear wave theory may not perfectly recover surface elevation signals. To solve this, field measurements were carried out to collect wave parameters at five observation stations, characterized by shallow to deep water environments. The data was uploaded to explain and solve this problem.通常而言，当前主流的线性波浪理论（linear wave theory）所采用的压力响应函数（pressure response function），难以完美还原水面高程信号（surface elevation signals）。针对该问题，研究团队开展现场实测工作，在5个覆盖浅水环境至深水环境的观测站点采集波浪参数。本数据集已公开上传，用于阐释并解决上述问题。