Articles | Volume 20, issue 3
https://doi.org/10.5194/tc-20-1497-2026
https://doi.org/10.5194/tc-20-1497-2026
Research article
 | 
09 Mar 2026
Research article |  | 09 Mar 2026

Active-source seismic characterization of subglacial lakes: numerical modeling, field validation, and implications for Antarctic exploration

Kai Lu and Yuqing Chen

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Cited articles

Agnew, R. S., Clark, R. A., Booth, A. D., Brisbourne, A. M., and Smith, A. M.: Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica, J. Glaciol., 1–12, https://doi.org/10.1017/jog.2023.82, 2023. a
Alkhalifah, T.: An acoustic wave equation for anisotropic media, Geophysics, 65, 1239–1250, 2000. a
Anandakrishnan, S. and Winberry, J.: Antarctic subglacial sedimentary layer thickness from receiver function analysis, Global and Planetary Change, 42, 167–176, 2004. a
Bentley, M., Christoffersen, P., Hodgson, D., Smith, A., Tulaczyk, S., and Le Brocq, A.: Subglacial lake sediments and sedimentary processes: potential archives of ice sheet evolution, past environmental change, and the presence of life, Antarctic Subglacial Aquatic Environments, 192, 83–110, 2011. a
Boiero, D., Wiarda, E., and Vermeer, P.: Surface-and guided-wave inversion for near-surface modeling in land and shallow marine seismic data, the Leading Edge, 32, 638–646, 2013. a
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Seismic imaging of subglacial lakes is affected by multiple reflections, guided waves, and source-side ghost effects, which dominate seismic records and complicate imaging. Using wavefield simulations under varied geological scenarios and real data analysis, this study clarifies how these effects arise and tests processing methods to reduce them. 

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