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Sliding-Law Parameter and Airborne Radar-Derived Basal Reflectivity Data Underneath Thwaites Glacier, Antarctica Data DOI: https://doi.org/10.15784/601658 Cite as Das, I. (2023) "Sliding-Law Parameter and Airborne Radar-Derived Basal Reflectivity Data Underneath Thwaites Glacier, Antarctica" U.S. Antarctic Program (USAP) Data Center. doi: https://doi.org/10.15784/601658. AMD - DIF Record(s) USAP-2152622_1 Abstract Data resulting from comparing model and observations of sliding-law parameter and airborne radar-derived basal reflectivity underneath Thwaites Glacier, Antarctica Creator(s): Das, Indrani Date Created: 2023-01-25 Repository: USAP-DC (current) License: Creative Commons Attribution Only v4.0 Generic [CC BY 4.0] Spatial Extent(s) West: -110, East: -100, South: -77, North: -74 Award(s) NSF 2152622 Version: 1 Related Project(s) NSF-NERC: PROcesses, drivers, Predictions: Modeling the response of Thwaites Glacier over the next Century using Ice/Ocean Coupled Models (PROPHET) References Das, I., Morlighem, M., Barnes, J., Gudmundsson, G. H., Goldberg, D., & Dias dos Santos, T. (2023). In the quest of a parametric relation between ice sheet model inferred Weertman's sliding-law parameter and airborne radar-derived basal reflectivity underneath Thwaites Glacier, Antarctica. Geophysical Research Letters, 50, e2022GL098910. (doi:10.1029/2022GL098910) Keywords Airborne Radar Antarctica Glaciers/ice Sheet Glaciology Thwaites Thwaites Glacier