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ESurf | Articles | Volume 6, issue 2
Earth Surf. Dynam., 6, 401–429, 2018
https://doi.org/10.5194/esurf-6-401-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Two centuries of modelling across scales (SE/ESurf inter-journal...

Earth Surf. Dynam., 6, 401–429, 2018
https://doi.org/10.5194/esurf-6-401-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Review article 29 May 2018

Review article | 29 May 2018

Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions

Pippa L. Whitehouse
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Cited articles  
A, G., Wahr, J., and Zhong, S. J.: Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada, Geophys. J. Int., 192, 557–572, https://doi.org/10.1093/Gji/Ggs030, 2013. 
Abe-Ouchi, A., Saito, F., Kawamura, K., Raymo, M. E., Okuno, J., Takahashi, K., and Blatter, H.: Insolation-driven 100 000-year glacial cycles and hysteresis of ice-sheet volume, Nature, 500, 190–193, https://doi.org/10.1038/nature12374, 2013. 
Adhikari, S. and Ivins, E. R.: Climate-driven polar motion: 2003–2015, Science Advances, 2, e1501693, https://doi.org/10.1126/sciadv.1501693, 2016. 
Adhikari, S., Ivins, E. R., Larour, E., Seroussi, H., Morlighem, M., and Nowicki, S.: Future Antarctic bed topography and its implications for ice sheet dynamics, Solid Earth, 5, 569–584, https://doi.org/10.5194/se-5-569-2014, 2014. 
Adhikari, S., Ivins, E. R., and Larour, E.: ISSM-SESAW v1.0: mesh-based computation of gravitationally consistent sea-level and geodetic signatures caused by cryosphere and climate driven mass change, Geosci. Model Dev., 9, 1087–1109, https://doi.org/10.5194/gmd-9-1087-2016, 2016. 
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This article is a contribution to a special issue on Two centuries of modelling across scales. It describes the historical observations, evolving hypotheses, and early calculations that led to the development of the field of glacial isostatic sdjustment (GIA) modelling, which seeks to understand feedbacks between ice-sheet change, sea-level change, and solid Earth deformation. Recent and future advances are discussed. Future progress will likely involve an interdisciplinary approach.
This article is a contribution to a special issue on Two centuries of modelling across scales....
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