North Atlantic climate and deep-ocean flow speed changes during the last 230 years
Variations in the near-bottom flow speed of Iceland-Scotland Overflow Water (ISOW) are documented in a 230-year-long deep-sea sediment record from the eastern flank of Reykjanes Ridge in the subpolar North Atlantic at (sub) decadal time scales. For recent decades, the ISOW palaeocurrent reconstructi...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
Amer Geophysical Union
2007
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Subjects: | |
Online Access: | https://doi.org/10.1029/2007GL030285 https://archimer.ifremer.fr/doc/00235/34646/33007.pdf https://archimer.ifremer.fr/doc/00235/34646/ |