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...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Boessenkool, K. P., Hall, I. R., Elderfield, H., Yashayaev, I.
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2007
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00235/34646/33007.pdf
https://doi.org/10.1029/2007GL030285
https://archimer.ifremer.fr/doc/00235/34646/