Under-ice acoustic communication in the Nansen Basin

P. V. van Walree, D. Tollefsen, Vidar Forsmo
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Abstract

An underwater acoustic experiment has been performed in the Nansen Basin (eastern Arctic) at $\mathbf{84}^{\circ}$ North. Channel probe signals and communication packets were transmitted in the 4–8 kHz band, with under-ice signaling over ranges of 10, 20 and 40 km. The measurements reveal a peculiarly sparse impulse response with two arrival groups, separated by 1–2 s, with contributions from surface duct arrivals, refracted paths, and bottom-reflected sound. A high propagation loss is counterbalanced by a low ambient noise level, yielding a useful SNR at all ranges. The main challenge for communications is the long impulse response, which causes a packet to collide not only with other packets transmitted over the same link, but also with itself. Some packets are lost because of these collisions, but there are also packets that are correctly received twice. Communication is possible over 40 km at a regular modem source level.
南森盆地冰下声通信
在南森盆地(北极东部)$\mathbf{84}^{\circ}$ North进行了水声实验。通道探测信号和通信数据包在4-8 kHz频段传输,冰下信号传输距离为10、20和40 km。测量结果显示,两个到达组的脉冲响应特别稀疏,间隔1-2秒,来自表面管道到达,折射路径和底部反射声音的贡献。高传播损耗被低环境噪声水平所抵消,从而在所有范围内产生有用的信噪比。通信的主要挑战是长脉冲响应,这不仅会导致数据包与同一链路上传输的其他数据包发生冲突,而且还会与自身发生冲突。有些数据包因为这些冲突而丢失,但也有数据包被正确接收两次。在常规调制解调器源电平下,通信可以超过40公里。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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