Udita Mukherjee

You have full access to this article via your institution. Addendum to: Nature Geoscience https://doi.org/10.1038/s41561-025-01806-0, published online 9 October 2025. Peter U. Clark has drawn our attention to the paper by Cuzzone et al. (2016) which, building on earlier work such as Carlson et al. (2008), came to a comparable conclusion about the meltwater partitioning between the North American and Antarctic ice sheets during the early Holocene.

Abstract The rapid transformation of the ocean–atmosphere–cryosphere system during the last deglaciation holds clues that may be useful to understand climate change during this century and beyond. Within this context, sea-level change connects the climate system components, but the limited temporal resolution and spatial distribution of relative sea-level records has hindered progress towards closing the ice sheet–sea-level budget since the Last Glacial Maximum.