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Role of measurement uncertainties in observed variability in the spectral backscattering ratio: a case study in mineral-rich coastal waters

机译:测量不确定性在光谱反向散射比的观测变化中的作用:以富含矿物质的沿海水域为例

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摘要

The particulate backscattering ratio (b_(bp)/b_(p)) is a useful indicator of the angular scattering characteristics of natural waters. Recent studies have shown evidence both for and against significant spectral variability in b_(bp)/b_(p) in the visible domain, but most show significant variability in its magnitude. We present results from a case study in which both backscattering and scattering coefficients were measured at nine wavelengths in a region of UK coastal waters where optical scattering is strongly influenced by inorganic particles and where a wide range of turbidities is found in a small geographic area. Using a new approach based on regression analysis of in situ signals, it is shown that, for this study site, most of the apparent variability in the magnitude of the backscattering ratio can be attributed to measurement uncertainties. Regression analysis suggests that b_(bp)/b_(p) is wavelength dependent for these mineral-rich waters. This conclusion can only be avoided by positing the existence of undocumented, systematic, wavelength-dependent errors in backscattering measurements made by two independently calibrated sensors. These results are important for radiative transfer simulations in mineral-dominated waters where the backscattering ratio has often been assumed to be spectrally flat. Furthermore, spectral dependence also has profound implications for our understanding of the relationship between b_(bp)/b_(p) and particle size distributions in coastal waters since the commonly assumed power-law distribution is associated with a spectrally flat particulate backscattering ratio for nonabsorbing particles.
机译:颗粒反向散射比(b_(bp)/ b_(p))是天然水角散射特性的有用指标。最近的研究表明,在可见域中,b_(bp)/ b_(p)的光谱可变性有明显的支持和反对,但大多数证据显示其幅度有明显的可变性。我们提供了一个案例研究的结果,其中在英国沿海水域的九个波长处同时测量了反向散射系数和散射系数,该区域的光学散射受到无机颗粒的强烈影响,并且在较小的地理区域内发现了大范围的浊度。使用一种基于原位信号回归分析的新方法,结果表明,对于该研究地点,大多数后向散射比的表观变异性可归因于测量不确定性。回归分析表明,对于这些富含矿物质的水,b_(bp)/ b_(p)与波长有关。只能通过在由两个独立校准的传感器进行的反向散射测量中存在未记录的,系统的,与波长相关的误差来避免该结论。这些结果对于矿物质为主的水域的辐射传输模拟非常重要,在矿物质为主的水域中,反向散射率通常被认为是频谱平坦的。此外,光谱依赖性还对我们对沿海水域b_(bp)/ b_(p)与粒径分布之间关系的理解产生了深远的影响,因为通常假定的幂律分布与非吸收的光谱平坦的颗粒反向散射比有关粒子。

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