Resumé
A diatom-based sea-ice transfer function was developed for the north-western Atlantic. A first reconstruction of sea-ice concentration off West Greenland shows multi-centennial oscillations superimposed an overall trend of expanding sea ice over the last 5000 years.
| Originalsprog | Engelsk |
|---|---|
| Sider (fra-til) | 24-25 |
| Antal sider | 2 |
| Tidsskrift | PAGES Magazine |
| Vol/bind | 23 |
| Udgave nummer | 1 |
| DOI | |
| Status | Udgivet - 2015 |
Programområde
- Programområde 5: Natur og klima