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电离层-空气-海水介质中水下VLF电磁波传播的HIE-FDTD方法OA

HIE-FDTD method for underwater VLF electromagnetic wave propagation in ionosphere-air-seawater media

中文摘要英文摘要

水下甚低频(very low frequency,VLF)电磁波在电离层-空气-海水介质中的传播研究对跨空海界面通信意义重大.针对精细分层结构,传统时域有限差分(finite-difference time-domain,FDTD)方法受最小网格限制,时间步长难以提升.本文提出采用混合隐式-显式时域有限差分(hybrid implicit-explicit finite-difference time-domain method,HIE-FDTD)方法预测水下 VLF 电磁波在电离层-空气-海水介质中的传播特性.推导了柱坐标系下完全匹配层(perfectly matched layer,PML)吸收边界中色散介质的 HIE-FDTD 迭代公式,构建了电离层-空气-海水三层介质中的水下VLF 源辐射电磁波传播模型,揭示电离层变化对水下及水上传播的影响.结果表明,HIE-FDTD 方法与传统 FDTD 方法精度相当,效率大幅提升;水下 VLF 源辐射电磁波在水下传播衰减剧烈且几乎不受电离层影响,水上空气中的传播则受电离层显著调制.白天电离层 D 层强吸收导致信号衰减加剧,夜间 D 层消失则显著改善传播条件,昼夜过渡中电离层参数渐变导致传播模式耦合转换,引起场强振荡及非均匀衰减.

The study of underwater very low frequency(VLF)electromagnetic wave propagation in ionosphere-air-seawater media is of great significance for cross-air-sea interface communication.For the fine-layered structure,the conventional finite-difference time-domain(FDTD)method was limited by the minimum grid size,making it difficult to increase the time step.In this paper,the hybrid implicit-explicit finite-difference time-domain(HIE-FDTD)method was proposed to predict the propagation characteristics of underwater VLF electromagnetic waves in ionosphere-air-seawater media.Iteration formulas of the HIE-FDTD method for dispersive media in the perfectly matched layer(PML)absorbing boundary were derived in cylindrical coordinates.A propagation model for electromagnetic waves radiated from an underwater VLF source in the three-layer ionosphere-air-seawater medium was constructed.The influence of ionospheric variations on underwater and above-water propagation was revealed.The results show that the HIE-FDTD method achieves comparable accuracy to the conventional FDTD method,with significantly improved efficiency.Underwater VLF waves radiated from a source attenuate severely and are almost unaffected by the ionosphere,while their propagation in the above-water air is significantly modulated by the ionosphere.Strong absorption by the daytime ionospheric D-layer leads to increased signal attenuation,whereas the disappearance of the D-layer at night significantly improves propagation conditions.During the day-night transition,gradual changes in ionospheric parameters cause mode coupling and conversion,resulting in significant oscillations and non-uniform attenuation of the field strength distribution.

王丹丹;徐凱华;孔文君;王东;李维新;蒲玉蓉

济南大学 信息科学与工程学院,济南 250022济南大学 信息科学与工程学院,济南 250022山东科技大学 电子信息工程学院,青岛 266590济南大学 信息科学与工程学院,济南 250022济南大学 信息科学与工程学院,济南 250022西安理工大学 自动化与信息工程学院,西安 710048

信息技术与安全科学

甚低频(VLF)电磁波传播时域有限差分(FDTD)混合隐式-显式时域有限差分(HIE-FDTD)完全匹配层(PML)色散介质

very low frequency(VLF)electromagnetic wave propagationfinite-difference time-domain(FDTD)hybrid implicit-explicit finite-difference time-domain(HIE-FDTD)perfectly matched layer(PML)dispersive media

《全球定位系统》 2026 (4)

10-17,8

国家自然科学基金重点项目(U2341201)国家自然科学基金面上项目(62571216)国家自然科学基金青年科学基金(62201326)山东省青年科技人才托举工程(SDAST2025QTA008)山东省高等学校青年创新团队(2025KJH090)

10.12265/j.gnss.2026199

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