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