基于GSM波束的有效大气-海洋跨介质传播模型的建立与研究

IF 4.3 Q1 OPTICS
Jiao Wang, Xuyan Tie, Zhenkun Tan, Sichen Lei, Pengfei Wu, Xianghui Wang, Lijun Deng
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引用次数: 0

摘要

以高斯-谢尔模型(GSM)光束为光源,基于扩展惠更斯-菲涅耳原理和线性滤波方法,建立了蓝-绿光束大气-海洋跨介质传播模型(AOCPM)。推导了GSM波束经过大气湍流、大气-海洋界面和海洋湍流后的交叉谱密度函数(CSDF)的封闭表达式。通过模拟不同参数下GSM波束在大气-海洋交叉介质中传播过程中强度、相对波束宽度和散斑归一化强度自相关函数的变化,验证了模型的正确性。结果表明:随着湍流强度和传播距离的增加,GSM波束在大气-海洋介质中传播后的强度呈类散斑高斯分布,波束强度逐渐衰减,相对波束宽度逐渐增大,散斑归一化强度自相关函数逐渐减小;此外,粗糙海面风速的增加主要导致强度的衰减。本文的工作为研究蓝绿光束的大气-海洋跨介质传播提供了新的思路。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Establishing and Investigating an Effective Atmosphere-Ocean Cross-Medium Propagation Model Based on GSM Beams

Establishing and Investigating an Effective Atmosphere-Ocean Cross-Medium Propagation Model Based on GSM Beams

Establishing and Investigating an Effective Atmosphere-Ocean Cross-Medium Propagation Model Based on GSM Beams

Establishing and Investigating an Effective Atmosphere-Ocean Cross-Medium Propagation Model Based on GSM Beams

Using the Gaussian-Schell model (GSM) beam as the light source, this study creates a blue-green beam atmosphere-ocean cross-medium propagation model (AOCPM) based on the extended Huygens-Fresnel principle and the linear filtering method. The closed expression of the Cross Spectral Density Function (CSDF) of the GSM beam after propagation through atmospheric turbulence, atmosphere-ocean interface, and ocean turbulence are derived. And the correctness of the model is verified by simulating the changes in intensity, relative beam width, and speckle normalized intensity autocorrelation function during the propagation of the GSM beam through the atmosphere-ocean cross-medium under different parameters. The findings demonstrate that the intensity of the GSM beam after being propagated through the atmosphere-ocean medium presents a speckle-like Gaussian distribution, the intensity of the GSM beam gradually attenuates, the relative beam width gradually grows, and the speckle normalized intensity autocorrelation function gradually decreases as the turbulence intensity and propagation distance increase. In addition, the increase in wind speed at rough sea surface mainly leads to the attenuation of intensity. The work of this paper provides a new idea for the study of atmosphere-ocean cross-medium propagation of blue-green beams.

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