Yang Jungang, Zhang Jie
The First Institute of Oceanography, Ministry of Natural Resources of China, Qingdao 266061, China.
Sensors (Basel). 2019 Jul 1;19(13):2914. doi: 10.3390/s19132914.
The validation of significant wave height (SWH) data measured by the Sentinel-3A/3B SAR Altimeter (SRAL) is essential for the application of the data in ocean wave monitoring, forecasting and wave climate studies. Sentinel-3A/3B SWH data are validated by comparisons with U. S. National Data Buoy Center (NDBC) buoys, using a spatial scale of 25 km and a temporal scale of 30 min, and with Jason-3 data at their crossovers, using a time difference of less than 30 min. The comparisons with NDBC buoy data show that the root-mean-square error (RMSE) of Sentinel-3A SWH is 0.30 m, and that of Sentinel-3B is no more than 0.31 m. The pseudo-Low-Resolution Mode (PLRM) SWH is slightly better than that of the Synthetic Aperture Radar (SAR) mode. The statistical analysis of Sentinel-3A/3B SWH in the bin of 0.5 m wave height shows that the accuracy of Sentinel-3A/3B SWH data decreases with increasing wave height. The analysis of the monthly biases and RMSEs of Sentinel-3A SWH shows that Sentinel-3A SWH are stable and have a slight upward trend with time. The comparisons with Jason-3 data show that SWH of Sentinel-3A and Jason-3 are consistent in the global ocean. Finally, the piecewise calibration functions are given for the calibration of Sentinel-3A/3B SWH. The results of the study show that Sentinel-3A/3B SWH data have high accuracy and remain stable.
哨兵-3A/3B合成孔径雷达高度计(SRAL)测量的有效波高(SWH)数据验证对于该数据在海浪监测、预报及海浪气候研究中的应用至关重要。哨兵-3A/3B的SWH数据通过与美国国家数据浮标中心(NDBC)浮标进行比较来验证,空间尺度为25千米,时间尺度为30分钟;在交叉点处与Jason-3数据进行比较,时间差小于30分钟。与NDBC浮标数据的比较表明,哨兵-3A的SWH均方根误差(RMSE)为0.30米,哨兵-3B的不超过0.31米。伪低分辨率模式(PLRM)的SWH略优于合成孔径雷达(SAR)模式。对波高0.5米区间内的哨兵-3A/3B的SWH进行统计分析表明,哨兵-3A/3B的SWH数据精度随波高增加而降低。对哨兵-3A的SWH月度偏差和RMSE分析表明,哨兵-3A的SWH稳定且随时间呈轻微上升趋势。与Jason-3数据的比较表明,哨兵-3A和Jason-3的SWH在全球海洋中是一致的。最后,给出了用于校准哨兵-3A/3B的SWH的分段校准函数。研究结果表明,哨兵-3A/3B的SWH数据具有高精度且保持稳定。