Abstract

Infrared ocean image simulation has been widely used in water-pollution prevention, meteorological observation and melting-ice monitoring. However, in actual remote sensing observation scenes, the simulation images provided by conventional algorithms are lacking sufficient wave details because the viewing angle and the scale of simulation images are simplex. In this paper, an infrared ocean image simulation algorithm based on the Pierson–Moskowitz spectrum and a bidirectional reflectance distribution function is proposed. First, a 3D model of ocean surface is set up based on Pierson–Moskowitz spectrum. Then, the imaging position is calculated by the pinhole camera imaging method, which describes how each point of the 3D model is mapping to the 2D image. Next, by using a bidirectional reflectance distribution function, the radiation intensity from every point of the ocean model to the camera is computed. Finally, we figure up the sum of the radiation intensity received by every point of the detector and obtain the infrared simulation ocean image by quantizing the radiation intensity sum to grayscale. The entropy of the simulation images is 2.725, which is, respectively, improved by 71.86% and 16.83% compared with two other algorithms. The Kullback–Leibler divergence of the simulation images is 11.446, which is improved by 0.54% and 0.59% compared with other algorithms. The quantitative experimental results prove that the authenticity and clarity of the presented simulation images have remarkable advantages over conventional algorithms.

Highlights

  • Infrared ocean image simulation algorithms play an important role in water-pollution prevention, meteorological observation and melting-ice monitoring

  • To solve the problem of lacking image authenticity and clarity, an infrared ocean image simulation algorithm based on the P-M spectrum and the bidirectional reflectance distribution function (BRDF) is proposed in this paper

  • To take into consideration the reflection of sun radiance and sky background radiance, we present a grayscale computing model based on the BRDF and pinhole camera imaging process to improve the authenticity of the simulation image

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Summary

Introduction

Infrared ocean image simulation algorithms play an important role in water-pollution prevention, meteorological observation and melting-ice monitoring. Chen et al [8] calculated the emissivity, reflectivity and the bidirectional reflectance of the sea surface by comparing the theoretical data with the measured data They applied the equivalent temperature method in the process of quantizing the radiation distribution into grayscale to obtain ocean images. To take into consideration the reflection of sun radiance and sky background radiance, we present a grayscale computing model based on the BRDF and pinhole camera imaging process to improve the authenticity of the simulation image.

Background
Theory of Infrared Ocean Image Simulation Algorithm
Reflection Model of Ocean Surface
Spontaneous Radiation Model of Ocean Surface
Imaging Model of Ocean Surface
Analysis of Simulation Images
Details and Parameter Setting
Qualitative Comparison
Quantitative Comparison
Conclusions
Full Text
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