航空三维云层析成像

Aviad Levis, Y. Schechner, Amit Aides, A. Davis
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引用次数: 69

摘要

我们试图在非均质介质中感知散射体的三维(3D)体积分布。研究这种介质的一个重要案例是大气。大气含量及其在地球辐射平衡中的作用在散射成分:气溶胶和云方面具有很大的不确定性。由水滴构成的云,也会导致降水和阴影等局部效应。我们的传感方法是使用被动多角度图像的计算机断层扫描。对于考虑多重散射的光-物质相互作用,我们使用三维辐射传递方程作为正演模型。在包含许多未知因素的大尺度下,通过反演该模型进行体积恢复存在计算瓶颈。所采取的步骤使该层析成像易于处理,而无需近似散射顺序或角度范围。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Airborne Three-Dimensional Cloud Tomography
We seek to sense the three dimensional (3D) volumetric distribution of scatterers in a heterogenous medium. An important case study for such a medium is the atmosphere. Atmospheric contents and their role in Earth's radiation balance have significant uncertainties with regards to scattering components: aerosols and clouds. Clouds, made of water droplets, also lead to local effects as precipitation and shadows. Our sensing approach is computational tomography using passive multi-angular imagery. For light-matter interaction that accounts for multiple-scattering, we use the 3D radiative transfer equation as a forward model. Volumetric recovery by inverting this model suffers from a computational bottleneck on large scales, which include many unknowns. Steps taken make this tomography tractable, without approximating the scattering order or angle range.
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