Shanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai 200030, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Sensors (Basel). 2021 Sep 12;21(18):6123. doi: 10.3390/s21186123.
The significant wave height (SWH) of oceans is the main parameter in describing the sea state, which has been widely used in the establishment of ocean process models and the field of navigation and transportation. However, traditional methods such as satellite radar altimeters and buoys cannot achieve SWH estimations with high spatial and temporal resolution. Recently, the spaceborne Global Navigation Satellite System reflectometry (GNSS-R) has provided an opportunity to estimate SWH with a rapid global coverage and high temporal resolution observations, particularly with the Cyclone Global Navigation Satellite System (CYGNSS) mission. In this paper, SWH was estimated using the polynomial function relationship between SWH from ERA5 and Delay-Doppler Map Average (DDMA) as well as Leading Edge Slope (LES) from CYGNSS data. Then, the SWH estimated from CYGNSS data was validated by ERA-Interim data, AVISO data, and buoy data. The results showed that the average correlation coefficient of CYGNSS SWH was 0.945, and the average RMSE was 0.257 m when compared to the ERA-Interim SWH data. The RMSE was 0.423 m and the correlation coefficient was 0.849 when compared with the AVISO SWH. The correlation coefficient with the buoy data was 0.907, and the RMSE was 0.247 m. This method can provide suitable SWH estimation data for ocean dynamics research and ocean environment prediction.
海洋的有效波高(SWH)是描述海况的主要参数,已广泛应用于海洋过程模型的建立以及航海和运输领域。然而,卫星雷达高度计和浮标等传统方法无法实现具有高时空分辨率的 SWH 估计。最近,星载全球导航卫星系统反射测量(GNSS-R)技术为快速全球覆盖和高时间分辨率观测提供了估计 SWH 的机会,尤其是 Cyclone Global Navigation Satellite System(CYGNSS)任务。本文使用从 ERA5 获得的 SWH 与从 CYGNSS 数据获得的延迟多普勒图平均(DDMA)和前缘斜率(LES)之间的多项式函数关系来估计 SWH。然后,使用 ERA-Interim 数据、AVISO 数据和浮标数据对从 CYGNSS 数据估计的 SWH 进行验证。结果表明,与 ERA-Interim SWH 数据相比,CYGNSS SWH 的平均相关系数为 0.945,平均均方根误差为 0.257 m。与 AVISO SWH 相比,均方根误差为 0.423 m,相关系数为 0.849。与浮标数据的相关系数为 0.907,均方根误差为 0.247 m。该方法可为海洋动力研究和海洋环境预测提供合适的 SWH 估计数据。