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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >A hybrid method to estimate suspended particle sizes from satellite measurements over Bohai Sea and Yellow Sea
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A hybrid method to estimate suspended particle sizes from satellite measurements over Bohai Sea and Yellow Sea

机译:一种混合方法,可根据渤海和黄海的卫星测量结果估算悬浮颗粒的大小

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摘要

Particle-size distribution (PSD), a measure of particle concentrations at different sizes, is of great importance to the understanding of many biogeochemical processes in coastal marine ecosystems. Here, a hybrid method, including analytical, semianalytical, and empirical steps, is developed to estimate PSD through the median diameter of suspended particles (D_v~(50)). Four cruise surveys were conducted to measure optical scattering properties, particle concentrations, spectral reflectance, and particle-size distributions (obtained with a LISST instrument covering a size range of 2.5–500 μm) in coastal waters of Bohai Sea, Yellow Sea, and Jiangsu coastal region. Based on the Mie scattering theory, D_v~(50) is closely related to massspecific backscattering coefficient of suspended particles (b_(bp)~*), and their relationship is calibrated through a power model (R~2=0.796, n=67, p<0.001) for the D_v~(50) range of 23.5–379.8 μm. The model is shown to perform better than the previously used inverse-proportion model. The retrieval of b_(bp)~* is through a bio-optical model that links remote sensing reflectance just beneath the surface to inherent optical properties, where a close empirical relationship is established between particulate backscattering and particle concentration. The hybrid method shows high degree of fitting (R~2=0.875, n=46, p<0.001) between the measured and estimated D_v~(50) for the size range of 17.2–325.2 μm used in the model calibration, while validation using two independent data sets shows mean absolute percentage errors of 46.0% and 64.7%, respectively. Application of the hybrid method to MODIS (Moderate Resolution Imaging Spectroradiometer) data results in spatial distributions of D_v~(50) that are generally consistent with those from in situ observations, suggesting potential use of the method in studying particle dynamics through time series of remote sensing observations. However, its general applicability to other regions still requires further research.
机译:粒度分布(PSD)是衡量不同大小的颗粒浓度的一种方法,对于理解沿海海洋生态系统中的许多生物地球化学过程非常重要。在此,开发了一种包括分析,半分析和经验步骤的混合方法,以通过悬浮颗粒的中值直径(D_v〜(50))估算PSD。在渤海,黄海和江苏沿海水域进行了四次巡航调查,以测量光学散射特性,粒子浓度,光谱反射率和粒度分布(使用覆盖范围为2.5–500μm的LISST仪器获得)沿海地区。基于米氏散射理论,D_v〜(50)与悬浮粒子的质量比背向散射系数(b_(bp)〜*)密切相关,并且它们之间的关系通过幂模型进行校正(R〜2 = 0.796,n = 67)。 (p <0.001),D_v〜(50)范围为23.5–379.8μm。该模型显示出比以前使用的反比例模型更好的性能。 b_(bp)〜*的获取是通过生物光学模型完成的,该模型将位于表面下方的遥感反射率与固有的光学特性相关联,在该光学特性中,颗粒的反向散射与颗粒浓度之间建立了紧密的经验关系。对于模型校准中使用的17.2–325.2μm尺寸范围,混合方法显示出实测值和估计值D_v〜(50)之间的高度拟合度(R〜2 = 0.875,n = 46,p <0.001)。使用两个独立的数据集显示的平均绝对百分比误差分别为46.0%和64.7%。将混合方法应用于MODIS(中等分辨率成像光谱仪)数据可得出D_v〜(50)的空间分布,该空间分布通常与原位观测的空间分布一致,这表明该方法在通过远程时间序列研究粒子动力学中的潜在用途感应观察。但是,其在其他地区的普遍适用性仍需进一步研究。

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