基于ARGO数据和激光传输特性的水下分层模型

Xiaohu Tang, Pengfei Zhang, Fang Lu, Xiang’e Han
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引用次数: 0

摘要

随着光电探测技术的发展,蓝绿激光水下传输与目标探测已成为一个研究热点。目前,大多数水下激光衰减通道模型都将海水视为均匀介质,少数分层模型只考虑叶绿素浓度随海水深度的变化,且层数较少。本文不仅考虑了叶绿素浓度的影响,还引入了温度和盐度的影响,增加了分层间隔数,改进了海水分层模型。根据中国实时地转海洋数据中心网站提供的海水垂直方向的温度、盐度和叶绿素浓度实测数据,给出了海水衰减系数的垂直分布。利用该分布对海水进行分层,建立了日本附近太平洋海域较为精确的海水垂直分层模型。利用本文建立的海水垂直分层模型,基于蒙特卡罗方法模拟了蓝绿激光在水下的传输过程。结果表明:随着传输距离的增加,分层海水中接收面上的光子包数始终大于均匀海水中的光子包数;分层海水情况下接收面上的光子包能量与均匀海水情况下的光子包能量交替增加,为激光在实际海水中的传输特性提供了参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Underwater stratified model based on ARGO data and laser transmission characteristics
With the development of photoelectric detection technology, blue-green laser underwater transmission and target detection have become a hot research field. At present, most of the underwater laser attenuation channel models regard seawater as a homogeneous medium, and a few layered models only consider the change of chlorophyll concentration with seawater depth, and the number of layers is small. This paper not only considers the influence of chlorophyll concentration, but also introduces the influence of temperature and salinity, increases the number of stratification intervals, and improves the seawater stratification model. Based on the measured data of temperature, salinity and chlorophyll concentration in the vertical direction of seawater provided by the Array for Real-time Geostrophic Oceanography data center website of China, the vertical distribution of seawater attenuation coefficient is given. Using this distribution, the seawater is stratified, and a more accurate vertical stratification model of seawater in the Pacific near Japan is established. Using the vertical stratification model of seawater established in this paper, the transmission process of blue-green laser underwater is simulated based on Monte Carlo method. The results show that with the increase of transmission distance, the number of photon packets on the receiving plane in layered seawater is always larger than that in uniform seawater. The photon packet energy on the receiving plane in the case of stratified seawater and the photon packet energy in the case of uniform seawater increase alternately, which provides a reference for the transmission characteristics of laser in actual seawater.
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