基于卫星遥感的海浪斜率方差验证与差异原因分析OA
Validation and Discrepancy Analysis of Sea Surface Mean Square Slope Measured by SWIM and CYGNSS
海面斜率方差 MSS(Mean Square Slope)是海洋微波遥感领域表征海面粗糙度的关键参数,对研究海气耦合过程及海洋气象监测意义重大.对中法海洋卫星 CFOSAT(China France Oceanography Satellite)搭载的海浪波谱仪 SWIM(Surface Waves Investigation and Monitoring)和旋风全球卫星导航系统 CYGNSS(Cyclone Global Navigation Satellite System)反演的 MSS展开对比分析.SWIM 通过拟合不同入射角和方位角下的二维归一化雷达后向散射截面反演 MSS,CYGNSS则在初步观测基础上减去一个校正量以获取局地风引起的 MSS.对 2023年 1月数据进行时空匹配后进行直接对比,发现小风速下 SWIM反演的 MSS大于 CYGNSS,而风速超过约 7 m·s-1 时,CYGNSS的 MSS大于 SWIM反演的 MSS,这主要归因于二者微波波段不同及 CYGNSS反演过程中减去涌浪产生的 MSS校正量.利用 Elfouhaily谱模型对 SWIM MSS校正后,二者平均偏差约为 0.03,随机均方误差为 0.0323,此误差源于涌浪产生的 MSS 及截止波长差异.研究结果明确了两种星载传感器反演 MSS的差异与误差来源,为MSS数据校准及后续海洋研究与应用提供了重要参考.
The Mean Square Slope(MSS)of the sea surface is a key parameter for characterizing sea surface roughness in the field of marine microwave remote sensing,and it is of great significance for studying the air-sea coupling process and marine meteorological monitoring.This paper conducts a com-parative analysis of the MSS retrieved by the Surface Waves Investigation and Monitoring(SWIM)on the China-France Oceanography Satellite(CFOSAT)and the Cyclone Global Navigation Satellite Sys-tem(CYGNSS).SWIM retrieves the MSS by fitting the two-dimensional normalized radar backscatter cross-section under different incident angles and azimuth angles.CYGNSS obtains the MSS caused by local winds by subtracting a correction amount on the basis of preliminary observations.In this paper,after collocating the data from SWIM and CYGNSS in January 2023,a direct comparison has been made.It is found that the MSS derived from SWIM is higher than that retrieved by CYGNSS under low wind speeds,while when the wind speed exceeds approximately 7 m·s-1,the MSS derived from CYGNSS is higher than that given by SWIM.This is mainly attributed to the differences in the microwave bands of the two and the correction amount of the MSS generated by swell subtracted during the retrieval pro-cess of CYGNSS.After correcting the SWIM MSS using the Elfouhaily spectrum model,the bias be-tween the two is approximately 0.03,and the random root mean square error is 0.0323.This error is caused by the MSS generated by swell and the differences in the cutoff wavelength.The research results clarify the differences and error sources of the MSS retrieved by the two spaceborne sensors,providing an important reference for the calibration of MSS data and subsequent marine research and applications.
郎姝燕;胡暐平;李秀仲;李雨阳;赵新华
国家卫星海洋应用中心 北京 100081||自然资源部空间海洋遥感与应用重点实验室 北京 100081南京信息工程大学海洋科学学院 南京 210044南京信息工程大学海洋科学学院 南京 210044||自然资源部空间海洋遥感与应用重点实验室 北京 100081南京信息工程大学海洋科学学院 南京 210044江苏海洋大学 江苏省海洋资源开发研究院 连云港 222001
海洋科学
海面斜率方差微波遥感中法海洋卫星海浪波谱仪旋风全球卫星导航系统
Sea surface mean square slopeMicrowave remote sensingCFOSATSurface Waves Investigation and Monitoring(SWIM)Cyclone Global Navigation Satellite System(CYGNSS)
《空间科学学报》 2026 (3)
718-725,8
国家自然科学基金重大项目(42192531)和山东省自然科学基金项目(ZR202102240074)共同资助
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