Abstract
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.
| Original language | English |
|---|---|
| Pages (from-to) | 24-25 |
| Number of pages | 2 |
| Journal | PAGES Magazine |
| Volume | 23 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 2015 |
Programme Area
- Programme Area 5: Nature and Climate
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