HY-1 C/D卫星CZI数据海面太阳耀光反射校正

Correction of Sunglint Reflection from Ocean Surface in HY-1 C/D CZI Images

  • 摘要: 水面耀光反射在海洋光学遥感中难以忽略,其差异有助于海洋目标监测,但会降低水色信息反演精度,因此耀光反射信号的精确计算或评估成为海洋遥感研究热点之一。受遥感尺度效应影响,适用于粗空间分辨率数据的耀光统计模型难以直接应用于高空间分辨率光学遥感数据。利用近红外-短波红外水体吸收特征的谱间关系法是实现高空间分辨率海洋光学数据太阳耀光校正的有效途径。以50 m空间分辨率的海洋一号C/D (HY-1 C/D)卫星海岸带成像仪(coastal zone imager,CZI)数据为对象,基于水面耀光反射的光学过程与海洋目标图像特征,分析了高空间分辨率海洋光学数据中耀光反射的图像特征及遥感尺度效应,并发展了相应的CZI耀光校正方法。结果表明,校正后CZI数据中涡旋、水团等水色信息得以凸显;受耀光反射影响的瑞利校正反射率(460 nm、560 nm和650 nm波段)的不确定性分别降低了65%、80%和89%。所提方法不依赖大气参数,有助于HY-1 C/D卫星CZI数据快速开展近海水色的动态监测与反演。

     

    Abstract:
    Objectives Sunglint is a significant phenomenon in marine optical remote sensing, and presents a dual character: its variability aids in marine target monitoring, yet it degrades the retrieval accuracy of water color information. Therefore, the precise calculation or assessment of sunglint signals has become a key research focus in ocean remote sensing. Affected by the remote sensing scale effect, statistical sunglint models suitable for coarse spatial resolution data are difficult to apply directly to high spatial resolution remote sensing data. The inter-band relationship approach, leveraging the absorption characteristics of water in the near-infrared (NIR) to shortwave infrared (SWIR) spectrum, provides an effective pathway for sunglint correction in high spatial resolution marine optical remote sensing data.
    Methods This paper utilizes data from the 50 m spatial resolution coastal zone imager (CZI) aboard the Haiyang-1 C/D (HY-1 C/D) satellites. Based on the optical processes of sunglint and the image characteristics of marine targets, we conducted a detailed analysis of the image features of sunglint and the remote sensing scale effects within high spatial resolution marine optical data. Furthermore, a dedicated sunglint correction method for CZI data was developed. The results demonstrate that post-correction CZI data effectively highlight water color information such as eddies and water masses.
    Results The uncertainty of Rayleigh correction affected by sunglint reflection at 460 nm, 560 nm, and 650 nm is reduced by 65%, 80%, and 89%, respectively.
    Conclusions The proposed method does not rely on atmospheric parameters, facilitating the rapid dynamic monitoring and retrieval of coastal water color using CZI data.

     

/

返回文章
返回