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Remote sensing estimation of colored dissolved organic matter (CDOM) in optically shallow waters

机译:光学浅水区有色溶解有机物(CDOM)的遥感估算

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It is not well understood how bottom reflectance of optically shallow waters affects the algorithm performance of colored dissolved organic matters (CDOM) retrieval. This study proposes a new algorithm that considers bottom reflectance in estimating CDOM absorption from optically shallow inland or coastal waters. The field sampling was conducted during four research cruises within the Saginaw River, Kawkawlin River and Saginaw Bay of Lake Huron. A stratified field sampling campaign collected water samples, determined the depth at each sampling location and measured optical properties. The sampled CDOM absorption at 440 nm broadly ranged from 0.12 to 8.46 m(-1). Field sample analysis revealed that bottom reflectance does significantly change water apparent optical properties. We developed a CDOM retrieval algorithm (Shallow water Bio-Optical Properties algorithm, SBOP) that effectively reduces uncertainty by considering bottom reflectance in shallow waters. By incorporating the bottom contribution in upwelling radiances, the SBOP algorithm was able to explain 74% of the variance of CDOM values (RMSE = 0.22 and R-2 = 0.74). The bottom effect index (BEI) was introduced to efficiently separate optically shallow and optically deep waters. Based on the BEI, an adaptive approach was proposed that references the amount of bottom effect in order to identify the most suitable algorithm (optically shallow water algorithm [SBOP] or optically deep water algorithm [QAA-CDOM]) to improve CDOM estimation (RMSE = 0.22 and R-2 = 0.81). Our results potentially help to advance the capability of remote sensing in monitoring carbon pools at the land-water interface. (C) 2017 International Society for Photogrammetry and Remote Sensing, Inc. (ISPRS). Published by Elsevier B.V. All rights reserved.
机译:尚不清楚光学浅水区的底部反射率如何影响有色溶解有机物(CDOM)检索的算法性能。这项研究提出了一种新算法,该算法在估计光学上较浅的内陆或沿海水域的CDOM吸收时考虑了底部反射率。野外采样是在萨吉诺河,卡考林河和休伦湖萨吉诺湾的四次研究航行中进行的。分层现场采样活动收集了水样,确定了每个采样位置的深度并测量了光学特性。在440 nm处采样的CDOM吸收范围从0.12到8.46 m(-1)。现场样品分析表明,底部反射率确实会显着改变水的表观光学性能。我们开发了一种CDOM检索算法(浅水生物光学特性算法,SBOP),该算法通过考虑浅水区的底部反射率来有效降低不确定性。通过将底部贡献合并到上升流辐射中,SBOP算法能够解释74%的CDOM值方差(RMSE = 0.22和R-2 = 0.74)。引入底部效应指数(BEI)可以有效地分离浅水和深水。在BEI的基础上,提出了一种自适应方法,该方法参考海底效应的数量以识别最合适的算法(光学浅水算法[SBOP]或光学深水算法[QAA-CDOM]),以改善CDOM估计(RMSE) = 0.22和R-2 = 0.81)。我们的研究结果可能有助于提高遥感监测陆地-水界面碳库的能力。 (C)2017国际摄影测量与遥感学会(ISPRS)。由Elsevier B.V.发布。保留所有权利。

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