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.
PNAS, 6 July 2026 Antarctic ice shelves act as natural barriers that slow the flow…
Nature Climate Change, 10 June 2026 Human-driven sea-level rise is transforming once-rare “extreme sea-level events”…
Advances in Climate Change Research, June 2026 Extratropical cyclones – large weather systems that transport…
Ocean Science, 30 June 2026 The North Sea has warmed about twice as fast as…
Environmental Research Climate, 3 July 2026 Glaciers in the Western Himalayas store vast freshwater reserves…
Climate Dynamics, 28 May 2026 Declining sea ice in the Arctic’s Barents-Kara Sea may be…