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PROTECT_policybrief2

anne.chapuis

Created on January 8, 2025

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Transcript

Policy recommendations

Key findings and recommendations

Factsheets

Acknowledgements

factsheets

Regional sea level change is different from the global average

Glaciers will keep losing mass, but we decide how fast and how much

Sea level is committed to rise until 2300 and beyond, but we can influence how much and how fast

Every glacierized region evolves differently under climate change, and so do the impacts

Navigating uncertainty: adapting to sea-level rise with flexible strategies

Ice shelf ocean melting and iceberg calving control the accelerated mass loss of the Antarctic Ice Sheet

Impacts and adaptation strategies for sea-level rise by 2150

Future sea level: the enduring legacy of Antarctic ice loss

Shaping tomorrow's coastlines: the long-term impact of sea-level rise

10

The Greenland Ice Sheet is losing its protective firn buffer, accelerating mass loss