TY - JOUR
T1 - Propagation-Model Fidelity for HED Localization in Multilayer Marine Media
AU - Liu, Jiahui
AU - Xue, Wei
AU - Bai, Xue
AU - Xu, Yidong
AU - Chen, Dijun
AU - Hu, Qiao
AU - Olshanskiy, Vladimir M.
AU - Zlenko, Dmitry V.
N1 - Publisher Copyright:
© 2002-2011 IEEE.
PY - 2026
Y1 - 2026
N2 - 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.
AB - 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.
KW - horizontal electric dipole
KW - matched-field processing
KW - multilayer marine media
KW - propagation-model mismatch
KW - source localization
KW - variable projection
KW - vertically stratified seawater
UR - https://www.scopus.com/pages/publications/105050163365
U2 - 10.1109/LAWP.2026.3731462
DO - 10.1109/LAWP.2026.3731462
M3 - 文章
AN - SCOPUS:105050163365
SN - 1536-1225
JO - IEEE Antennas and Wireless Propagation Letters
JF - IEEE Antennas and Wireless Propagation Letters
ER -