用神经网络方法估计PACE任务测量的水中衰减与吸收比

Jacopo Agagliate, Robert Foster, A. Ibrahim, A. Gilerson
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引用次数: 2

摘要

导言:为了准备即将到来的PACE任务,我们探索了一种基于神经网络的方法的可行性,该方法将HARP2仪器在大气顶部进行的线性极化程度的测量转换为海洋表层衰减与吸收比的估计。与仅基于遥感反射率的方法相比,偏振已被证明包含有关水中固有光学特性的信息,包括总衰减系数,这些方法仅限于散射的后向散射部分。反过来,这些特性可以进一步与反演算法相结合,以检索海洋颗粒的光学和物理特性的投影值。方法:使用生物光学模型生成足够数量的用于网络训练目的的合成数据,并使用从矢量辐射传输模型中导出的相关偏振值,我们生成了一个两步算法,首先检索表面水平偏振,其次检索衰减吸收比,每一步由单独的神经网络处理。这些网络使用多光谱输入,根据偏振计的线偏振度和海洋颜色仪器的遥感反射率,预计在PACE数据环境中完全可用。结果和讨论:产生的结果与预期值比较有利,表明神经网络介导的遥感极化转化为水中IOPs是可行的。对PACE轨道和HARP2视场的模拟进一步表明,即使在一次PACE过境期间地球表面任何给定点的数据点数量有限的情况下,这些结果也是可靠的。
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A neural network approach to the estimation of in-water attenuation to absorption ratios from PACE mission measurements
Introduction: In preparation for the upcoming PACE mission, we explore the feasibility of a neural network-based approach for the conversion of measurements of the degree of linear polarization at the top of the atmosphere as carried out by the HARP2 instrument into estimations of the ratio of attenuation to absorption in the surface layer of the ocean. Polarization has been shown to contain information on the in-water inherent optical properties including the total attenuation coefficient, in contrast with approaches solely based on remote sensing reflectance that are limited to the backscattered fraction of the scattering. In turn, these properties may be further combined with inversion algorithms to retrieve projected values for the optical and physical properties of marine particulates. Methodology: Using bio-optical models to produce synthetic data in quantities sufficient for network training purposes, and with associated polarization values derived from vector radiative transfer modeling, we produce a two-step algorithm that retrieves surface-level polarization first and attenuation-to-absorption ratios second, with each step handled by a separate neural network. The networks use multispectral inputs in terms of the degree of linear polarization from the polarimeter and the remote sensing reflectance from the Ocean Color Instrument that are anticipated to be fully available within the PACE data environment. Result and Discussion: Produce results that compare favorably with expected values, suggesting that a neural network-mediated conversion of remotely sensed polarization into in-water IOPs is viable. A simulation of the PACE orbit and of the HARP2 field of view further shows these results to be robust even over the limited number of data points expected to be available for any given point on Earth’s surface over a single PACE transit.
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