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Relationships between the surface concentration of particulate organic carbon and optical properties in the eastern South Pacific and eastern Atlantic Oceans

机译:南太平洋东部和大西洋东部颗粒有机碳的表面浓度与光学性质的关系

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We have examined several approaches for estimating the surface concentrationof particulate organic carbon, POC, from optical measurements of spectralremote-sensing reflectance, Rrs(λ), using field datacollected in tropical and subtropical waters of the eastern South Pacific andeastern Atlantic Oceans. These approaches include a direct empiricalrelationship between POC and the blue-to-green band ratio of reflectance,RrsB)/Rrs(555), and two-step algorithmsthat consist of relationships linking reflectance to an inherent opticalproperty IOP (beam attenuation or backscattering coefficient) and POC to theIOP. We considered two-step empirical algorithms that exclusively includepairs of empirical relationships and two-step hybrid algorithms that consistof semianalytical models and empirical relationships. The surface POC in ourdata set ranges from about 10 mg m−3 within the South PacificSubtropical Gyre to 270 mg m−3 in the Chilean upwelling area, andancillary data suggest a considerable variation in the characteristics ofparticulate assemblages in the investigated waters. The POC algorithm basedon the direct relationship between POC andRrsB)/Rrs(555) promises reasonably goodperformance in the vast areas of the open ocean covering different provincesfrom hyperoligotrophic and oligotrophic waters within subtropical gyres toeutrophic coastal upwelling regimes characteristic of eastern oceanboundaries. The best error statistics were found for power function fits tothe data of POC vs. Rrs(443)/Rrs(555) and POCvs. Rrs(490)/Rrs(555). For our data set thatincludes over 50 data pairs, these relationships are characterized by themean normalized bias of about 2% and the normalized root mean square errorof about 20%. We recommend that these algorithms be implemented for routineprocessing of ocean color satellite data to produce maps of surface POC withthe status of an evaluation data product for continued work on algorithmdevelopment and refinements. The two-step algorithms also deserve furtherattention because they can utilize various models for estimating IOPs fromreflectance, offer advantages for developing an understanding of bio-opticalvariability underlying the algorithms, and provide flexibility for regionalor seasonal parameterizations of the algorithms.
机译:我们使用热带地区收集的野外数据,研究了几种通过光谱遥感反射反射率 R rs (λ)的光学测量来估算颗粒有机碳POC表面浓度的方法。和南太平洋东部和大西洋东部的亚热带水域。这些方法包括POC与反射率的蓝绿色比, R rs (λ B < / sub>)/ R rs (555),以及两步算法,该算法包括将反射率与固有光学特性IOP(光束衰减或后向散射系数)和POC关联起来的关系IOP。我们考虑了仅包含成对的经验关系的两步经验算法以及由半分析模型和经验关系组成的两步​​混合算法。我们数据集中的地表POC范围从南太平洋亚热带环流内的大约10 mg m −3 到智利上升流区的270 mg m −3 ,并且辅助数据表明被调查水域中微粒组合特征的变化。基于POC与 R rs (λ B )/ R < sub> rs (555)承诺在从亚热带回旋区内的超营养性和贫营养性水域到东部海洋边界具有特征的富营养性沿海上升体制,在覆盖不同省份的广阔海洋中均具有相当好的性能。对于POC与 R rs (443)/ R rs 的数据,幂函数拟合的最佳误差统计被找到i>(555)和POCvs。 R rs (490)/ R rs (555)。对于我们的数据集(包括50多个数据对),这些关系的特征在于归一化偏差约为2%,归一化均方根误差约为20%。我们建议将这些算法用于海洋彩色卫星数据的例行处理,以生成具有评估数据产品状态的地表POC图,以便继续进行算法开发和完善。两步算法也值得进一步关注,因为它们可以利用各种模型来从反射率估计IOP,为进一步理解算法基础的生物光学可变性提供优势,并为算法的区域或季节参数化提供了灵活性。

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