一种改进的水下图像形成模型

D. Akkaynak, T. Treibitz
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引用次数: 172

摘要

目前的水下图像形成模型来源于大气除雾方程,其中衰减是波长的弱函数。我们最近表明,该模型在直接传输信号的估计中引入了显着的误差和依赖性,因为在水下,光以波长相关的方式衰减。在这里,我们表明,从当前模型导出的后向散射信号也受到以前未考虑的依赖关系的影响。在此过程中,我们使用海洋学测量来推导物理上有效的后向散射空间,并进一步表明,控制后向散射的宽带系数与控制直接传输的宽带系数不同,尽管目前的模型认为它们是相同的。我们提出了一个考虑到这些差异的水下图像形成修正方程,并通过水下原位实验对其进行了验证。修正后的模型可以解释当前水下颜色重建模型的频繁不稳定性,并呼吁开发新的方法。
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A Revised Underwater Image Formation Model
The current underwater image formation model descends from atmospheric dehazing equations where attenuation is a weak function of wavelength. We recently showed that this model introduces significant errors and dependencies in the estimation of the direct transmission signal because underwater, light attenuates in a wavelength-dependent manner. Here, we show that the backscattered signal derived from the current model also suffers from dependencies that were previously unaccounted for. In doing so, we use oceanographic measurements to derive the physically valid space of backscatter, and further show that the wideband coefficients that govern backscatter are different than those that govern direct transmission, even though the current model treats them to be the same. We propose a revised equation for underwater image formation that takes these differences into account, and validate it through in situ experiments underwater. This revised model might explain frequent instabilities of current underwater color reconstruction models, and calls for the development of new methods.
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