O. Kuznietsov, Oleksii Kolomiitsev, Ivan Nos, O. Biesova, Heorhii Krykhovetskyi
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The results of experimental studies of seasonal and daily changes in the parameters of the lower troposphere layer in the Black Sea coastal zone and the parameters of tropospheric radio waveguides are presented. The procedure for calculating the energy transmission losses during radio wave propagation in the boundary layer of the atmosphere is presented, and the conditions for detecting SO and AO beyond the radar line-of-sight are determined. Recommendations for increasing the range of detection of SO and AO are given, which are associated with the possibility of predicting the existence of tropospheric radio waveguides by using data on the current conditions of radio wave propagation over the sea based on the signals of the automatic ship identification system AIS. Conclusions. Proposals have been developed to improve the accuracy of measuring the range and radial velocity of SO and AO at waveguide propagation of radio waves over the sea surface. A promising area for further research may be to identify ways to optimise the measurement of angular coordinates in modern RS during waveguide propagation of radio waves over the sea surface.","PeriodicalId":275587,"journal":{"name":"Advanced Information Systems","volume":"48 11","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-02-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"PROPOSALS TO IMPROVE THE INFORMATION CAPABILITIES OF COASTAL-BASED RADAR STATIONS FOR SURVEILLANCE OF SURFACE AND AIR OBJECTS\",\"authors\":\"O. Kuznietsov, Oleksii Kolomiitsev, Ivan Nos, O. Biesova, Heorhii Krykhovetskyi\",\"doi\":\"10.20998/2522-9052.2024.1.06\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Sea-based radar stations (RS) are widely used for solving the tasks of radar surveillance of surface objects (SO) and air objects (AO). 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Recommendations for increasing the range of detection of SO and AO are given, which are associated with the possibility of predicting the existence of tropospheric radio waveguides by using data on the current conditions of radio wave propagation over the sea based on the signals of the automatic ship identification system AIS. Conclusions. Proposals have been developed to improve the accuracy of measuring the range and radial velocity of SO and AO at waveguide propagation of radio waves over the sea surface. 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引用次数: 0
摘要
海基雷达站(RS)被广泛用于解决雷达监视水面物体(SO)和空中物体(AO)的任务。文章的主题是无线电波在大气边界层中的传播机制。目的是研究提高测量沿岸 RS 视线外观测到的 SO 和 AO 的距离和径向速度精度的可能性。目标:分析水面以上波导层的时空参数和特性。采用的方法:最大似然法和频率法。结果如下介绍了对黑海沿岸地区对流层下层参数和对流层无线电波导参数的季节变化和日变化的实验研究结果。介绍了无线电波在大气边界层传播期间能量传输损失的计算程序,并确定了在雷达视线之外探测 SO 和 AO 的条件。提出了扩大 SO 和 AO 探测范围的建议,这些建议与利用基于船舶自动识别系统 AIS 信号的海上无线电波传播现状数据预测对流层无线电波导存在的可能性有关。结论。已经提出了一些建议,以提高在海面无线电波传播波导处测量 SO 和 AO 的距离和径向速度的精度。进一步研究的一个有前途的领域可能是确定在无线电波在海面上的波导传播过程中优化现代 RS 角坐标测量的方法。
PROPOSALS TO IMPROVE THE INFORMATION CAPABILITIES OF COASTAL-BASED RADAR STATIONS FOR SURVEILLANCE OF SURFACE AND AIR OBJECTS
Sea-based radar stations (RS) are widely used for solving the tasks of radar surveillance of surface objects (SO) and air objects (AO). The subject of the article is the mechanisms of radio wave propagation in the boundary layer of the atmosphere. The aim is to investigate the possibilities of improving the accuracy of measuring the range and radial velocity of SO and AO observed beyond the line-of-sight of coastal-based RS. Objective: to analyse the spatial and temporal parameters and properties of waveguide layers above the water surface. Methods used: maximum likelihood and frequency. The following results were obtained. The results of experimental studies of seasonal and daily changes in the parameters of the lower troposphere layer in the Black Sea coastal zone and the parameters of tropospheric radio waveguides are presented. The procedure for calculating the energy transmission losses during radio wave propagation in the boundary layer of the atmosphere is presented, and the conditions for detecting SO and AO beyond the radar line-of-sight are determined. Recommendations for increasing the range of detection of SO and AO are given, which are associated with the possibility of predicting the existence of tropospheric radio waveguides by using data on the current conditions of radio wave propagation over the sea based on the signals of the automatic ship identification system AIS. Conclusions. Proposals have been developed to improve the accuracy of measuring the range and radial velocity of SO and AO at waveguide propagation of radio waves over the sea surface. A promising area for further research may be to identify ways to optimise the measurement of angular coordinates in modern RS during waveguide propagation of radio waves over the sea surface.