Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
The major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet's dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 y from localities far from former ice
|Collections||ANU Research Publications|
|Source:||PNAS - Proceedings of the National Academy of Sciences of the United States of America|
|01_Lambeck_Sea_level_and_global_ice_2014.pdf||1.11 MB||Adobe PDF|
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