{"title":"Improving Retrieval of Sea Surface Roughness From Landsat-8 OLI and Sentinel-2 MSI Imagery by Eliminating for Ambiguity Effects","authors":"Chen Wang;Huaguo Zhang;Guanghong Liao;Wenting Cao;Juan Wang;Dongling Li;Xiulin Lou","doi":"10.1109/TGRS.2024.3499964","DOIUrl":null,"url":null,"abstract":"Sea surface roughness (SSR) is a common metric used to characterize the condition of sea surfaces. Sun glitter (SG) is the reflected sunlight off the fluctuating sea surface, with its distribution and intensity markedly influenced by SSR. However, the estimation of SSR through single-angle SG images may produce ambiguity, due to the assumptions applied in the underlying statistical model describing the orientation of the sea surface facets as a function of wind speed. In this study, we investigate the causes of SSR ambiguity and its distribution characteristics via simulation experiments. Based on these findings, we propose a method for identifying critical points of ambiguity and eliminating them for SSR estimation, leveraging single-angle SG images. This approach enables pixel-scale adaptive quantitative inversion of SSR. To validate our model, publicly available global high-resolution SG images (near-infrared (NIR) and shortwave infrared (SWIR) bands) captured by the Landsat-8 Operational Land Imager (OLI) and Sentinel-2 MultiSpectral Instrument sensors are utilized for SSR estimation. Subsequently, the modal values of SSR are expressed as wind-speed values for accuracy assessment. The estimated wind speeds exhibit good agreement with reanalysis wind data from the European Centre for Medium-Range Weather Forecasting (ECMWF) and buoy wind data from the National Data Buoy Center (NDBC). Meanwhile, the comparison results of the two bands are also very consistent, indicating that the method is stable for application on NIR and SWIR bands. The model’s efficacy is demonstrated using typical oceanographic scenarios from two regions: the Timor Sea and the English Channel. The resulting SSR images depict detailed oceanographic features with minimal noise, showcasing quantitative SSR changes at the pixel level. These outcomes underscore the effectiveness of the proposed method in resolving SSR ambiguity inherent in widely used optical remote sensing images such as Landsat-8 and Sentinel-2, thereby enhancing SSR retrieval accuracy.","PeriodicalId":13213,"journal":{"name":"IEEE Transactions on Geoscience and Remote Sensing","volume":"62 ","pages":"1-13"},"PeriodicalIF":8.6000,"publicationDate":"2024-11-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"IEEE Transactions on Geoscience and Remote Sensing","FirstCategoryId":"5","ListUrlMain":"https://ieeexplore.ieee.org/document/10755122/","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, ELECTRICAL & ELECTRONIC","Score":null,"Total":0}
引用次数: 0
Abstract
Sea surface roughness (SSR) is a common metric used to characterize the condition of sea surfaces. Sun glitter (SG) is the reflected sunlight off the fluctuating sea surface, with its distribution and intensity markedly influenced by SSR. However, the estimation of SSR through single-angle SG images may produce ambiguity, due to the assumptions applied in the underlying statistical model describing the orientation of the sea surface facets as a function of wind speed. In this study, we investigate the causes of SSR ambiguity and its distribution characteristics via simulation experiments. Based on these findings, we propose a method for identifying critical points of ambiguity and eliminating them for SSR estimation, leveraging single-angle SG images. This approach enables pixel-scale adaptive quantitative inversion of SSR. To validate our model, publicly available global high-resolution SG images (near-infrared (NIR) and shortwave infrared (SWIR) bands) captured by the Landsat-8 Operational Land Imager (OLI) and Sentinel-2 MultiSpectral Instrument sensors are utilized for SSR estimation. Subsequently, the modal values of SSR are expressed as wind-speed values for accuracy assessment. The estimated wind speeds exhibit good agreement with reanalysis wind data from the European Centre for Medium-Range Weather Forecasting (ECMWF) and buoy wind data from the National Data Buoy Center (NDBC). Meanwhile, the comparison results of the two bands are also very consistent, indicating that the method is stable for application on NIR and SWIR bands. The model’s efficacy is demonstrated using typical oceanographic scenarios from two regions: the Timor Sea and the English Channel. The resulting SSR images depict detailed oceanographic features with minimal noise, showcasing quantitative SSR changes at the pixel level. These outcomes underscore the effectiveness of the proposed method in resolving SSR ambiguity inherent in widely used optical remote sensing images such as Landsat-8 and Sentinel-2, thereby enhancing SSR retrieval accuracy.
通过消除模糊效应改进 Landsat-8 OLI 和 Sentinel-2 MSI 图像的海面粗糙度检索
海面粗糙度(SSR)是描述海面状况的常用指标。太阳闪光(SG)是波动海面反射的阳光,其分布和强度受 SSR 的显著影响。然而,通过单角度 SG 图像估算 SSR 可能会产生歧义,这是由于描述海面切面方位的基础统计模型与风速之间函数关系的假设所致。在本研究中,我们通过模拟实验研究了 SSR 模糊性的原因及其分布特征。基于这些发现,我们提出了一种方法,利用单角 SG 图像来识别模糊临界点并消除它们,从而进行 SSR 估计。这种方法可实现像素尺度的 SSR 自适应定量反演。为了验证我们的模型,我们利用陆地卫星 8 号业务陆地成像仪(OLI)和哨兵 2 号多光谱仪器传感器拍摄的公开全球高分辨率 SG 图像(近红外和短波红外波段)来估算 SSR。随后,将 SSR 的模态值表示为风速值,以进行精度评估。估算的风速与欧洲中期天气预报中心(ECMWF)的再分析风速数据和国家数据浮标中心(NDBC)的浮标风速数据具有良好的一致性。同时,两个波段的对比结果也非常一致,表明该方法在近红外和西南红外波段的应用是稳定的。该模型的功效通过帝汶海和英吉利海峡两个区域的典型海洋场景得到了验证。生成的 SSR 图像以最小的噪声描绘了详细的海洋特征,展示了像素级的 SSR 定量变化。这些成果强调了所提方法在解决 Landsat-8 和 Sentinel-2 等广泛使用的光学遥感图像中固有的 SSR 模糊性方面的有效性,从而提高了 SSR 检索的准确性。
期刊介绍:
IEEE Transactions on Geoscience and Remote Sensing (TGRS) is a monthly publication that focuses on the theory, concepts, and techniques of science and engineering as applied to sensing the land, oceans, atmosphere, and space; and the processing, interpretation, and dissemination of this information.