Sea-level rise results from a combination of several processes, from polar ice sheet loss to mountain glacier melt and more. Structured in a dynamic format, this COP29 event asked audience members to test their knowledge about sea-level rise with experts from the major cryosphere dynamics that drive sea-level rise. Speakers included Dr. Florence Colleoni, SCAR and the Italian National Institute of Oceanography and Applied Geophysics; Dr. David Rounce, Carnegie Mellon University; Dr. Bella Rowell, ICCI’s Antarctica Director; and Dr. James Kirkham, Chief Science Advisor to the Ambition on Melting Ice (AMI) High-level Group.
Philosophical Transactions of the Royal Society, 23 April 2026 Observations suggest we are currently tracking…
NPJ Natural Hazards, 16 April 2026) Rising temperatures and shifting regional precipitation patterns are reducing…
Nature Communications, 18 March 2026 This study identified a marked increase in both flood frequency…
The Cryosphere, 7 April 2026 Projections of Antarctica’s response to temporary but extreme ocean warming…
The Cryosphere, 1 April 2026 Antarctic sea ice stayed fairly steady from 2010-2014, but began…
Changes in Antarctica can trigger fast and cascading impacts, often with global consequences. Multiple abrupt…