Resumé
Sea ice is an integral component of the climate system, but a difficult one to reconstruct. Biochemical tracers preserved in marine sediments now reveal the waxing and waning of sea ice since the Last Glacial Maximum in an Arctic Ocean gateway.
Originalsprog | Engelsk |
---|---|
Sider (fra-til) | 743-744 |
Antal sider | 2 |
Tidsskrift | Nature Geoscience |
Vol/bind | 2 |
Udgave nummer | 11 |
DOI | |
Status | Udgivet - nov. 2009 |
Programområde
- Programområde 5: Natur og klima