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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/10.15784/601744 Cite as Emry, E. (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/10.15784/601744. AMD - DIF Record(s) USAP-1643873_1 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. These results were presented by Emry and Hansen at the 2022 Fall Meeting of the American Geophysical Union. Creator(s): Emry, Erica Date Created: 2023-10-16 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: 1 Related Project(s) Collaborative Research: Imaging Seismic Heterogeneity within the Antarctic Mantle with Full Waveform Ambient Noise Tomography Keywords Ambient Seismic Noise Antarctica Full-Waveform Inversion Seismic Tomography Shear Wave Velocity Solid Earth