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Propagation-Model Fidelity for HED Localization in Multilayer Marine Media

  • Jiahui Liu
  • , Wei Xue
  • , Xue Bai
  • , Yidong Xu
  • , Dijun Chen
  • , Qiao Hu
  • , Vladimir M. Olshanskiy
  • , Dmitry V. Zlenko
  • Harbin Engineering University
  • Xi'an Jiaotong University
  • Russian Academy of Sciences

Research output: Contribution to journal › Article › peer-review

Abstract

Underwater electromagnetic localization can interpret propagation-model error as source displacement. We quantify this effect for single-frequency horizontal electric-dipole localization in vertically stratified marine media. The model hierarchy progresses from unbounded uniform water (H0), through bounded uniform water (W1), to profile-resolved water columns. A fast Fourier transform–Sommerfeld solver and variable-projection matched-field estimator separate boundary and vertical-profile effects while eliminating unknown source coefficients. At 30 dB, adding air and seabed reduces three-dimensional root-mean-square error from 23.079–27.584 m for H0 to 0.495–0.535 m for W1. Resolving the nominal eight-layer profile further lowers error from 0.486–0.575 to 0.094–0.108 m. The improvement is not pointwise monotone and becomes calibration-dependent. Under an independent WOA18 profile extending to 350 m, a seven-layer approximation reduces the circular-layout median from 1.224 to 0.749 m. It reduces the square-layout median from 1.010 to 0.628 m. Adverse pairs and a shared depth ambiguity remain. External boundaries therefore remove gross bias, whereas vertical resolution supplies a conditional correction governed by profile accuracy, frequency, geometry, and calibration.

Original languageEnglish
JournalIEEE Antennas and Wireless Propagation Letters
DOIs
StateAccepted/In press - 2026
Externally publishedYes

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 14 - Life Below Water
    SDG 14 Life Below Water

Keywords

  • horizontal electric dipole
  • matched-field processing
  • multilayer marine media
  • propagation-model mismatch
  • source localization
  • variable projection
  • vertically stratified seawater

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