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Mid-frequency acoustic transmission and communication in the Arctic: the Nansen Basin under-ice experiments

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The Arctic Ocean's rapidly changing environment necessitates robust measurement and monitoring capabilities, often relying on acoustic communication under ice cover. This paper presents validated data from under-ice acoustic transmission experiments conducted in the Nansen Basin (August 2019 and March 2023), revealing complex signal propagation influenced by oceanographic ducts and water depths. Measured impulse responses, ranging from 8 to 42 nautical miles, demonstrate the interplay of direct, surface-ducted, and bottom-reflected paths.
Mid-frequency acoustic transmission and communication in the Arctic: the Nansen Basin under-ice experiments

The Arctic Ocean’s rapidly changing environment necessitates increasingly sophisticated monitoring and measurement capabilities, a challenge highlighted by recent research into under-ice acoustic communication. This paper, detailing experiments conducted in the Nansen Basin, underscores the complexities of utilizing acoustics for data transmission in this challenging environment. The findings have significant implications for deploying and operating oceanographic platforms reliant on acoustic communication, particularly as the Arctic continues to warm and its ice cover diminishes. Understanding acoustic propagation under ice is critical for a range of applications, from tracking marine mammals to deploying autonomous underwater vehicles (AUVs) for scientific research, and even for potential future resource exploration. These challenges are compounded by the inherent variability of Arctic conditions, as discussed in “The thermal gap constraint: why satellite degree heating weeks fail where reefs need them most,” which demonstrates the limitations of established predictive models in specific regions – a parallel illustrating the need for localized, empirically-driven data collection. The interplay between ice thickness, water temperature, and salinity creates unique acoustic propagation channels, a phenomenon this research meticulously investigates.

The study's findings, detailing the complex interplay of direct, surface-ducted, and bottom-reflected acoustic paths, are particularly noteworthy. The observation that bottom-reflected arrivals can either degrade modem performance or, conversely, enable error-free decoding, highlights the nuanced nature of acoustic communication in the Arctic. This reinforces the need for adaptive communication strategies that can leverage these varied propagation paths. Furthermore, the reliance on numerical modeling, validated by empirical data, demonstrates a commitment to scientific rigor essential for advancing our understanding. Such rigorous methodologies are vital in the context of increasingly complex environmental challenges, mirroring the need for unbiased scientific negotiation of marine resources discussed in “The future of our oceans: negotiating marine fisheries, aquaculture, and living resources with unbiased science.” The experimental design, incorporating data from both August 2019 and March 2023, provides valuable longitudinal data reflecting seasonal variations in ice and ocean conditions, offering a more comprehensive picture of acoustic behavior. The use of coherent multiband modulation as a successful communication scheme further underscores the importance of innovative technological approaches to overcome the limitations imposed by the Arctic environment. Even geopolitical considerations impacting oceanic research, as showcased by the recent events involving the oil tanker in "EU Forces Board Oil Tanker Suspected Of Sailing Under False Flag In Mediterranean Sea," highlight the increased scrutiny and complexity of operating in these regions.

The implications of this research extend beyond simply improving communication reliability for existing oceanographic platforms. As the Arctic becomes increasingly accessible due to climate change, the need for robust, real-time data collection will only intensify. This includes monitoring changes in ice thickness, ocean currents, and water chemistry, all of which are critical for understanding the broader impacts of climate change on Arctic ecosystems and global climate patterns. The integrated data ecosystem concept, allowing for the seamless combination of various data streams, is paramount – acoustically-derived data is one crucial piece of this puzzle. Calibrated acoustic measurements, combined with other validated data sources, can provide a more holistic picture of the Arctic system, contributing to more accurate predictive models and informed decision-making regarding resource management and environmental protection. Longitudinal data collection, as demonstrated in this study, is vital for establishing baselines and detecting long-term trends, allowing for adaptive management strategies and early warnings of potential ecological shifts.

Ultimately, this research serves as a valuable contribution to the growing body of knowledge regarding acoustic propagation in the Arctic. The demonstrated ability to accurately model and interpret complex acoustic signals under ice provides a foundation for developing more reliable and efficient communication systems for future Arctic operations. The question moving forward is how we can effectively integrate these empirically-derived insights with broader climate models and predictive tools to improve our understanding of the Arctic’s role in the global climate system and to inform responsible stewardship of this rapidly changing region.

The Arctic Ocean is undergoing rapid environmental changes, and measurement and monitoring of its physical ice-ocean variables is becoming increasingly important. To operate under conditions of ice cover, oceanographic measurement platforms must typically rely on acoustics for communication and navigation, and it is of interest to explore limitations for such. In this context, this paper presents data from mid-frequency (0.5-1.7 kHz and 4–8 kHz) under-ice acoustic transmission and communication experiments at two sites in the Nansen Basin of the Arctic Ocean, in August 2019 and March 2023, respectively. The areas of experiment were characterized by stable ice-cover (78% and 99% ice concentration, respectively), under-ice oceanographic ducts (depths ~25–180 m) and water depths 2700–4000 m. Measured impulse responses at ranges of 8, 21, and 42 nmi showed considerable delay spread between distinct groups of arrivals due to direct, surface-ducted, and bottom-reflected paths. The relative strengths of these groups depend on duct and under-ice properties, and source-receiver range. In general, in-duct paths at shallow grazing angles are attenuated with range due to repeated under-ice reflection loss, while bottom-reflected paths can remain strong to longer range. The interpretations of impulse responses are supported by numerical modeling using the Bellhop ray model with an under-ice reflection model that includes rough-surface scattering. Of the tested communication schemes, a coherent multiband modulation performed best in these Arctic environments. Bottom-reflected arrivals play an important role in this analysis. They can either degrade modem performance by interfering with the surface-ducted reception or enable error free decoding of the bottom reflection alone.

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