Wei Jianwei, Lee Zhongping
Appl Opt. 2015 Feb 1;54(4):636-49. doi: 10.1364/AO.54.000636.
The light absorption of phytoplankton and colored detrital matter (CDM), which includes contribution of gelbstoff and detrital matters, has distinctive yet overlapping features in the ultraviolet (UV) and visible domain. The CDM absorption (a(dg)) increases exponentially with decreasing wavelength while the absorption coefficient of phytoplankton (a(ph)) generally decreases toward the shorter bands for the range of 350-450 nm. It has long been envisioned that including ocean color measurements in the UV range may help the separation of these two components from the remotely sensed ocean color spectrum. An attempt is made in this study to provide an analytical assessment of this expectation. We started with the development of an absorption decomposition model [quasi-analytical algorithm (QAA)-UV], analogous to the QAA, that partitions the total absorption coefficient using information at bands 380 and 440 nm. Compared to the retrieval results relying on the absorption information at 410 and 440 nm of the original QAA, our analyses indicate that QAA-UV can improve the retrieval of a(ph) and a(dg), although the improvement in accuracy is not significant for values at 440 nm. The performance of the UV-based algorithm is further evaluated with in situ measurements. The limited improvement observed with the field measurements highlights that the separation of a(dg) and a(ph) is highly dependent on the accuracy of the ocean color measurements and the estimated total absorption coefficient.
浮游植物和有色碎屑物质(CDM,包括黄色物质和碎屑物质)的光吸收在紫外(UV)和可见光波段具有独特但重叠的特征。CDM吸收(a(dg))随波长减小呈指数增加,而浮游植物的吸收系数(a(ph))在350 - 450 nm范围内通常向较短波段减小。长期以来,人们一直设想在紫外波段进行海洋颜色测量可能有助于从遥感海洋颜色光谱中分离这两种成分。本研究试图对这一预期进行分析评估。我们首先开发了一种吸收分解模型[准分析算法(QAA)-UV],类似于QAA,它利用380和440 nm波段的信息对总吸收系数进行划分。与依赖原始QAA的410和440 nm吸收信息的反演结果相比,我们的分析表明QAA-UV可以改进a(ph)和a(dg)的反演,尽管对于440 nm处的值,精度提高并不显著。基于紫外的算法性能通过现场测量进一步评估。现场测量观察到的有限改进突出表明,a(dg)和a(ph)的分离高度依赖于海洋颜色测量的精度和估计的总吸收系数。