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1. Antarctic ice sheet sensitivity to atmospheric CO 2 variations in the early to mid-Miocene

   https://doi.org/10.1073/pnas.1516030113  

   Levy, Richard ; Harwood, David ; Florindo, Fabio ; Sangiorgi, Francesca ; Tripati, Robert ; von Eynatten, Hilmar ; Gasson, Edward ; Kuhn, Gerhard ; Tripati, Aradhna ; DeConto, Robert ; et al ( March 2016 , Proceedings of the National Academy of Sciences)
2. Solid Earth change and the evolution of the Antarctic Ice Sheet

   https://doi.org/10.1038/s41467-018-08068-y  

   Whitehouse, Pippa L. ; Gomez, Natalya ; King, Matt A. ; Wiens, Douglas A. ( December 2019 , Nature Communications)
3. The impact of 3-D Earth structure on far-field sea level following interglacial West Antarctic Ice Sheet collapse

   https://doi.org/10.1016/j.quascirev.2021.107256  

   Powell, Evelyn M. ; Pan, Linda ; Hoggard, Mark J. ; Latychev, Konstantin ; Gomez, Natalya ; Austermann, Jacqueline ; Mitrovica, Jerry X. ( December 2021 , Quaternary Science Reviews)
4. The Influence of the Solid Earth on the Contribution of Marine Sections of the Antarctic Ice Sheet to Future Sea‐Level Change

   https://doi.org/10.1029/2021GL097525  

   Yousefi, M. ; Wan, J. ; Pan, L. ; Gomez, N. ; Latychev, K. ; Mitrovica, J. X. ; Pollard, D. ; DeConto, R. M. ( August 2022 , Geophysical Research Letters)

   Seismic tomography models indicate highly variable Earth structure beneath Antarctica with anomalously low shallow mantle viscosities below West Antarctica. An improved projection of the contribution of the Antarctic Ice Sheet to sea‐level change requires consideration of this complexity to precisely account for water expelled into the ocean from uplifting marine sectors. Here we build a high‐resolution 3‐D viscoelastic structure model based on recent inferences of seismic velocity heterogeneity below the continent. The model serves as input to a global‐scale sea‐level model that we use to investigate the influence of solid Earth deformation in Antarctica on future global mean sea‐level (GMSL) rise. Our calculations are based on a suite of ice mass projections generated with a range of climate forcings and suggest that water expulsion from the rebounding marine basins contributes 4%–16% and 7%–14% to the projected GMSL change at 2100 and 2500, respectively.

    

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5. A Coupled Ice Sheet–Sea Level Model Incorporating 3D Earth Structure: Variations in Antarctica during the Last Deglacial Retreat

   https://doi.org/10.1175/JCLI-D-17-0352.1  

   Gomez, Natalya ; Latychev, Konstantin ; Pollard, David ( May 2018 , Journal of Climate)