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Application of the Support Vector Regression Method for Turbidity Assessment with MODIS on a Shallow Coral Reef Lagoon (Voh-Koné-Pouembout, New Caledonia)

机译:支持向量回归法在浅层珊瑚礁泻湖(新喀里多尼亚Voh-Koné-Pouembout)浊度评估中的应用

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Particle transport by erosion from ultramafic lands in pristine tropical lagoons is a crucial problem, especially for the benthic and pelagic biodiversity associated with coral reefs. Satellite imagery is useful for assessing particle transport from land to sea. However, in the oligotrophic and shallow waters of tropical lagoons, the bottom reflection of downwelling light usually hampers the use of classical optical algorithms. In order to address this issue, a Support Vector Regression (SVR) model was developed and tested. The proposed application concerns the lagoon of New Caledonia—the second longest continuous coral reef in the world—which is frequently exposed to river plumes from ultramafic watersheds. The SVR model is based on a large training sample of in-situ turbidity values representative of the annual variability in the Voh-Koné-Pouembout lagoon (Western Coast of New Caledonia) during the 2014–2015 period and on coincident satellite reflectance values from MODerate Resolution Imaging Spectroradiometer (MODIS). It was trained with reflectance and two other explanatory parameters—bathymetry and bottom colour. This approach significantly improved the model’s capacity for retrieving the in-situ turbidity range from MODIS images, as compared with algorithms dedicated to deep oligotrophic or turbid waters, which were shown to be inadequate. This SVR model is applicable to the whole shallow lagoon waters from the Western Coast of New Caledonia and it is now ready to be tested over other oligotrophic shallow lagoon waters worldwide.
机译:原始热带泻湖中超镁铁质土地侵蚀造成的颗粒运输是一个关键问题,特别是对于与珊瑚礁相关的底栖生物和中上层生物多样性而言。卫星图像对于评估从陆地到海洋的粒子传输非常有用。但是,在热带泻湖的贫营养和浅水域,井下光线的底部反射通常会阻碍经典光学算法的使用。为了解决此问题,开发并测试了支持向量回归(SVR)模型。拟议中的申请涉及新喀里多尼亚泻湖(世界上第二长的连续珊瑚礁),该泻湖经常暴露于超镁铁质分水岭的河羽中。 SVR模型基于大量浊度值的训练样本,这些浊度值代表了2014-2015年期间Voh-Koné-Pouembout泻湖(新喀里多尼亚西海岸)的年度变化,并基于MODerate的卫星反射率值分辨率成像光谱仪(MODIS)。使用反射率和其他两个解释性参数(测深法和底色)进行了训练。与专用于深层贫营养或浑浊水的算法相比,这种方法显着提高了模型从MODIS图像中检索原位浊度范围的能力,而后者被证明是不够的。该SVR模型适用于新喀里多尼亚西海岸的整个泻湖浅水区,现在已经可以在全球其他贫营养化的泻湖浅水区进行测试。

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