Long-term variations in Iceland–Scotland overflow strength during the Holocene
The overflow of deep water from the Nordic seas into the North Atlantic plays a critical role in global ocean circulation and climate. Approximately half of this overflow occurs via the Iceland–Scotland (I–S) overflow, yet the history of its strength throughout the Holocene (~ 0–11 700 yr ago, ka) i...
| Main Authors: | , , , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2013-09-01
|
| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/9/2073/2013/cp-9-2073-2013.pdf |