Variations of North Atlantic inflow to the central Arctic Ocean over the last 14 million years inferred from hafnium and neodymium isotopes
The warm and saline North Atlantic inflow to the Arctic Ocean is a major component of high northern latitude circulation and the main mechanism of deep water renewal in the Arctic Ocean. Knowledge of its past variability is critical for understanding the high latitude feedback mechanisms of the clim...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
2012-11-01.
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| Subjects: | |
| Online Access: | Get fulltext |