ISMIP6-based Antarctic projections to 2100: simulations with the BISICLES ice sheet model
<p>The contribution of the Antarctic Ice Sheet is one of the most uncertain components of sea level rise to 2100. Ice sheet models are the primary tool for projecting future sea level contribution from continental ice sheets. The Ice Sheet Model Intercomparison for the Coupled Model Intercompa...
Saved in:
Main Authors: | J. F. O'Neill, T. L. Edwards, D. F. Martin, C. Shafer, S. L. Cornford, H. L. Seroussi, S. Nowicki, M. Adhikari, L. J. Gregoire |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2025-02-01
|
Series: | The Cryosphere |
Online Access: | https://tc.copernicus.org/articles/19/541/2025/tc-19-541-2025.pdf |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Sustainability of regional Antarctic ice sheets under late Eocene seasonal atmospheric conditions
by: D. H. A. Vermeulen, et al.
Published: (2025-01-01) -
Plausible Last Interglacial Antarctic Ice Sheet Changes Do Not Fully Explain Antarctic Ice Core Water Isotope Records
by: Huiling Zou, et al.
Published: (2025-01-01) -
Evidence of active subglacial lakes under a slowly moving coastal region of the Antarctic Ice Sheet
by: J. F. Arthur, et al.
Published: (2025-01-01) -
Present-day mass loss rates are a precursor for West Antarctic Ice Sheet collapse
by: T. van den Akker, et al.
Published: (2025-01-01) -
Signal characteristics of surface seismic explosive sources near the West Antarctic Ice Sheet divide
by: Marianne S. Karplus, et al.
Published: (2024-01-01)