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Impact of Dynamic Ocean-Atmosphere Interface on Quantum Communication Performance

Yufeng Yanga, Wuchuandong Pei, Yi jun Zhang

Published Jan 1, 2025• 0 citations
Publisher
DOI
10.2139/ssrn.5584111

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Impact of dynamic ocean-atmosphere interface on quantum communication performance

Yufeng Yang, Wuchuandong Pei, Yijun Zhang

Quantum communication at the sea-air interface is an important direction for expanding quantum information networks. However, current research has not sufficiently considered how waves and bubbles at this interface affect quantum communication. The paper develops a system combining the Cox-Munk sea surface wave model with the Hall-Novarini bubble scattering model, using Monte Carlo simulations to model photon propagation in air-sea channels. Based on data for different wind speeds (5–20 m/s) and four water types (pure, clear, coastal, harbor), the study examines how the sea-air interface influences quantum bit error rate (QBER) and received power for quantum communication. Results show that in pure seawater, higher wind speeds decrease the maximum secure communication depth from 63 m to 25 m. In waters with high turbidity, scattering effects dominate, limiting communication depth to within 10 m. This research identifies environmental thresholds for marine quantum channels, offering a theoretical basis and practical guidelines for designing and improving underwater quantum communication systems.

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Performance of Ship-Based QKD Under the Influence of Sea-Surface Atmospheric Turbulence

Guiying Jiang, Yaping Li, Xiao-Han Li +5 more

There are numerous studies on the effects of ocean turbulence on wireless optical communications and on satellite–ground quantum key distribution (QKD); however, there are few studies on the impact of near sea-surface turbulence on ship-based QKD performance. This study investigates the influence of sea-surface atmospheric turbulence on laser beam propagation, atmospheric scintillation, and aiming error. It focuses on the impact of sea-surface turbulence on the performance of satellite-to-ship QKD and ship-to-ship QKD systems. The results show that strong turbulence severely degrades QKD system performance; horizontal transmission distances change from 32 km (weak turbulence) to 3 km (strong turbulence) in ship-to-ship QKD.

Photonics•Apr 3, 2025•3 citations
Quantum communication at the sea-air interface is an important direction for expanding quantum information networks. However, current research has not sufficiently considered how waves and bubbles at this interface affect quantum communication. The paper develops a system combining the Cox-Munk sea surface wave model with the Hall-Novarini bubble scattering model, using Monte Carlo simulations to model photon propagation in air-sea channels. Based on data for different wind speeds (5–20 m/s) and four water types (pure, clear, coastal, harbor), the study examines how the sea-air interface influences quantum bit error rate (QBER) and received power for quantum communication. Results show that in pure seawater, higher wind speeds decrease the maximum secure communication depth from 63 m to 25 m. In waters with high turbidity, scattering effects dominate, limiting communication depth to within 10 m. This research identifies environmental thresholds for marine quantum channels, offering a theoretical basis and practical guidelines for designing and improving underwater quantum communication systems.
There are numerous studies on the effects of ocean turbulence on wireless optical communications and on satellite–ground quantum key distribution (QKD); however, there are few studies on the impact of near sea-surface turbulence on ship-based QKD performance. This study investigates the influence of sea-surface atmospheric turbulence on laser beam propagation, atmospheric scintillation, and aiming error. It focuses on the impact of sea-surface turbulence on the performance of satellite-to-ship QKD and ship-to-ship QKD systems. The results show that strong turbulence severely degrades QKD system performance; horizontal transmission distances change from 32 km (weak turbulence) to 3 km (strong turbulence) in ship-to-ship QKD.