Preprints
https://doi.org/10.5194/egusphere-2024-2957
https://doi.org/10.5194/egusphere-2024-2957
08 Nov 2024
 | 08 Nov 2024
Status: this preprint is open for discussion.

The impact of regional-scale upper mantle heterogeneity on glacial isostatic adjustment in West Antarctica

Erica Margaret Lucas, Natalya Gomez, and Terry Wilson

Abstract. West Antarctica is underlain by a laterally heterogenous upper mantle, with localized regions of mantle viscosity reaching several orders of magnitude below the global average. Accounting for 3-D viscosity variability in glacial isostatic adjustment (GIA) simulations has been shown to impact the predicted spatial rates and patterns of crustal deformation, geoid, and sea level changes in response to surface ice loading changes. Uncertainty in the viscoelastic structure of the solid Earth remains a major limitation in GIA modeling. To date, investigations of the impact of 3-D Earth structure on GIA have adopted solid Earth viscoelastic models based on global- and continental-scale seismic imaging, with variability at spatial length scales > 150 km. However, regional body-wave tomography shows mantle structure variability at smaller length scales (~50–100 km) in central West Antarctica. Here, we investigate the effects of incorporating smaller-scale lateral variability in upper mantle viscosity into 3-D GIA simulations. Lateral variability in upper mantle structure at the glacial drainage basin scale is found to impact GIA model predictions for modern and projected ice mass changes, especially in coastal regions that undergo rapid ice mass loss. Differences between simulations adopting upper mantle viscosity structure inferred from regional- versus coarser continental-scale seismic imaging are large enough to impact the interpretation of crustal motion observations and reach up to ~15 % of the total predicted sea level change during the instrumental record. Incorporating a strong transition from lower viscosities at the mouth of the Thwaites and Pine Island glaciers to higher viscosities in the interior of the glacier basins results in a ~10–20 % difference in predicted sea level change in the vicinity of the grounding line over the next ~300 years. These findings have a range of implications for the interpretation of geophysical observables and improving constraints on feedbacks between the West Antarctic Ice Sheet and the solid Earth.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Erica Margaret Lucas, Natalya Gomez, and Terry Wilson

Status: open (until 22 Dec 2024)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2957', Anonymous Referee #1, 06 Dec 2024 reply
Erica Margaret Lucas, Natalya Gomez, and Terry Wilson
Erica Margaret Lucas, Natalya Gomez, and Terry Wilson

Viewed

Total article views: 132 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
96 30 6 132 20 1 2
  • HTML: 96
  • PDF: 30
  • XML: 6
  • Total: 132
  • Supplement: 20
  • BibTeX: 1
  • EndNote: 2
Views and downloads (calculated since 08 Nov 2024)
Cumulative views and downloads (calculated since 08 Nov 2024)

Viewed (geographical distribution)

Total article views: 125 (including HTML, PDF, and XML) Thereof 125 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 09 Dec 2024
Download
Short summary
We investigate the effects of incorporating regional-scale lateral variability (~50–100 km) in upper mantle structure into models of Earth deformation and sea level change associated with ice mass changes in West Antarctica. Regional-scale variability in upper mantle structure is found to impact relative sea level and crustal rate predictions for modern (last ~25–125 years) and projected (next ~300 years) ice mass changes, especially in coastal regions that undergo rapid ice mass loss.