Articles | Volume 21, issue 9
https://doi.org/10.5194/cp-21-1611-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-21-1611-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evaluation of regional climate features over Antarctica in the PMIP past1000 experiment and implications for 21st-century sea level rise
Vincent Charnay
CORRESPONDING AUTHOR
Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand
Daniel P. Lowry
Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand
Department of Surface Geosciences, GNS Science, Lower Hutt, New Zealand
College of Marine Science, University of South Florida, St Petersburg, FL, USA
Elizabeth D. Keller
Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand
Department of Surface Geosciences, GNS Science, Lower Hutt, New Zealand
Abha Sood
Centre of Sustainability, University of Otago, Dunedin, New Zealand
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Beata Bukosa, Sara Mikaloff-Fletcher, Gordon Brailsford, Dan Smale, Elizabeth D. Keller, W. Troy Baisden, Miko U. F. Kirschbaum, Donna L. Giltrap, Lìyǐn Liáng, Stuart Moore, Rowena Moss, Sylvia Nichol, Jocelyn Turnbull, Alex Geddes, Daemon Kennett, Dóra Hidy, Zoltán Barcza, Louis A. Schipper, Aaron M. Wall, Shin-Ichiro Nakaoka, Hitoshi Mukai, and Andrea Brandon
Atmos. Chem. Phys., 25, 6445–6473, https://doi.org/10.5194/acp-25-6445-2025, https://doi.org/10.5194/acp-25-6445-2025, 2025
Short summary
Short summary
We used atmospheric measurements and inverse modelling to estimate New Zealand's carbon dioxide (CO2) emissions and removals from 2011 to 2020. Our study reveals that New Zealand's land absorbs more CO2 than previously estimated, particularly in areas dominated by indigenous forests. Our results highlight gaps in current national CO2 estimates and methods, suggesting a need for further research to improve emissions reports and refine approaches to track progress toward climate mitigation goals.
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Short summary
Our study evaluates models' ability to simulate Antarctic regional climate features by comparing available Paleoclimate Modelling Intercomparison Project models to sets of Last Millennium Antarctic proxy-based reconstructions most relevant to the surface mass balance. We later look at their implications for 21st-century sea level rise. The best-scoring model predicts a higher surface mass balance by 2100, which implies stronger mitigation of the ice sheet contribution to sea level rise.
Our study evaluates models' ability to simulate Antarctic regional climate features by comparing...