利用Bahía Blanca站点的AERONET-OC数据对Landsat OLI图像进行大气校正和浊度反演的验证

Maximiliano Arena, A. L. Delgado, P. Pratolongo, Carla Celleri, Alejandro J. Vitale
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引用次数: 1

摘要

AERONET-OC从全球分布的自主CE-318太阳光度计收集数据,这些太阳光度计适用于测量来自海洋的辐射(即离开水的辐射)。该网络通过使用单一测量系统和协议在不同地点进行标准化测量,支持卫星海洋颜色验证活动。2020年1月,在Bahía布兰卡河口的主要航道口建立了Bahía布兰卡站点,这是一个复杂的系统,广泛的侵蚀和强烈的潮流是通道中典型的高悬浮载荷的原因。在这项工作中,我们基于AERONET-OC数据和手持光谱辐射计获得的现场测量数据,对该地区Landsat-OLI场景的大气校正进行了三种不同算法的验证。利用地表遥感反射率反演卫星浊度,并利用与卫星立交桥同时采集的水样浊度测量数据对算法性能进行了测试。根据我们的研究结果,基于黑像元假设的大气校正算法获得了最佳拟合,使用两个OLI-SWIR波段估计气溶胶类型,并允许空间变化(每像元变量epsilon)。气溶胶类型沿河口方向变化,epsilon参数通常从河口内侧开始减小。卫星浊度原位测量回归线性能良好(R2 = 0.97, n=20),精度高(RMSE = 4.03, NMAE= 0.16),无高估或低估倾向(BIAS = 0.63)。将经过适当验证的算法应用于高空间分辨率图像的卫星数据,可以识别河口的浊度特征,这是由河岸和湍流上的再悬浮现象引起的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Validation of the atmospheric correction of Landsat OLI imagery and turbidity retrievals using AERONET-OC data from the Bahía Blanca site
AERONET-OC collects data from worldwide distributed autonomous CE-318 sun-photometers adapted to provide measurements of the radiance emerging from the sea (i.e., water-leaving radiance). The network supports satellite ocean color validation activities through standardized measurements performed at different sites with a single measuring system and protocol. In January 2020 the Bahía Blanca site was established at the mouth of the main navigation channel of the Bahía Blanca Estuary, a complex system where widespread erosion and strong tidal currents are responsible for the typically high suspended loads in the channel. In this work we present a validation of three different algorithms for the atmospheric correction of Landsat-OLI scenes over the area, based on AERONET-OC data and in situ measurements obtained with a hand-held spectroradiometer. Surface remote sensing reflectance was used to retrieve satellite turbidity and the algorithm performance was tested using turbidity measurements obtained from water samples collected simultaneously with satellite overpasses. According to our results, the best fit was obtained with the atmospheric correction algorithm based on the black-pixel assumption, with the aerosol type estimated using the two OLI-SWIR bands and allowed to vary spatially (per pixel variable epsilon). The aerosol type changed along the estuary, with an epsilon parameter that commonly decreased from the inner section through the mouth. The regression line of in situ measurements with satellite turbidity showed a good performance (R2 = 0.97, n=20), with a high accuracy (RMSE = 4.03, NMAE= 0.16) and no tendency to over or underestimation (BIAS = 0.63). The application of properly validated algorithms to satellite data from high spatial resolution images allowed for the identification of detailed turbidity features in the estuary, resulting from re-suspension phenomena over banks and turbulent currents.
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