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Shear Wave Velocity of the Antarctic Upper Mantle from Full Waveform Inversion and Long Period Ambient Seismic Noise Data DOI: https://doi.org/10.15784/601909 Cite as Emry, E., & Hansen, S. (2023) "Shear Wave Velocity of the Antarctic Upper Mantle from Full Waveform Inversion and Long Period Ambient Seismic Noise" U.S. Antarctic Program (USAP) Data Center. doi: https://doi.org/10.15784/601909. Abstract This dataset provides the shear-wave velocity model resulting from a full-waveform inversion that was constrained using long-period empirical Green's functions extracted from ambient seismic noise. The results are highlighted in Hansen and Emry (2025). Creator(s): Emry, Erica; Hansen, Samantha Date Created: 2025-02-27 Repository: USAP-DC (current) License: Creative Commons Attribution Only v4.0 Generic [CC BY 4.0] Spatial Extent(s) West: -180, East: 180, South: -90, North: -60 Award(s) NSF 1643798 NSF 1643873 Version: 2 Related Project(s) Collaborative Research: Imaging Seismic Heterogeneity within the Antarctic Mantle with Full Waveform Ambient Noise Tomography References S.E. Hansen and E.L. Emry, East Antarctic tectonic basin structure and its implications for ice-sheet modeling and sea-level projections. Nature Comm. Earth Environ. (doi:10.1038/s43247-025-02140-4) Keywords Ambient Seismic Noise Antarctica Antarctica Cryosphere Full-Waveform Inversion Seismic Tomography Shear Wave Velocity