La fracture Gibbs et la circulation profonde en Atlantique Nord
The cold waters from the Norwegian Sea are the main source of the underflow system in the northern Atlantic Ocean (10) (pl. 1, fig. 1b). The role of these currents in the formation of large sediment ripples has been demonstrated in some recent studies [(2), (3)]. As in the southern Atlantic Ocean, t...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | French |
Published: |
Académie des Sciences
1970
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Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/1970/publication-4882.pdf https://archimer.ifremer.fr/doc/00000/4882/ |