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