- Home
- Search Results
- Page 1 of 1
Search for: All records
-
Total Resources3
- Resource Type
-
00030
- Availability
-
30
- Author / Contributor
- Filter by Author / Creator
-
-
Susan Lozier, M. (3)
-
Bower, Amy S. (2)
-
Xu, Xiaobiao (2)
-
Zou, Sijia (2)
-
Bacon, Sheldon (1)
-
Bower, Amy (1)
-
Cunningham, Stuart A. (1)
-
Drouin, Kimberley L. (1)
-
Femke de Jong, M. (1)
-
Fischer, Jürgen (1)
-
Furey, Heather (1)
-
Furey, Heather H. (1)
-
Gary, Stefan F. (1)
-
Greenan, Blair J. (1)
-
Heimbach, Patrick (1)
-
Holliday, Naomi P. (1)
-
Houpert, Loïc (1)
-
Inall, Mark E. (1)
-
Johns, William E. (1)
-
Johnson, Helen L. (1)
-
- Filter by Editor
-
-
& Spizer, S. M. (0)
-
& . Spizer, S. (0)
-
& Ahn, J. (0)
-
& Bateiha, S. (0)
-
& Bosch, N. (0)
-
& Brennan K. (0)
-
& Brennan, K. (0)
-
& Chen, B. (0)
-
& Chen, Bodong (0)
-
& Drown, S. (0)
-
& Ferretti, F. (0)
-
& Higgins, A. (0)
-
& J. Peters (0)
-
& Kali, Y. (0)
-
& Ruiz-Arias, P.M. (0)
-
& S. Spitzer (0)
-
& Spitzer, S. (0)
-
& Spitzer, S.M. (0)
-
(submitted - in Review for IEEE ICASSP-2024) (0)
-
- (0)
-
-
Have feedback or suggestions for a way to improve these results?
!
Note: When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher.
Some full text articles may not yet be available without a charge during the embargo (administrative interval).
What is a DOI Number?
Some links on this page may take you to non-federal websites. Their policies may differ from this site.
-
Zou, Sijia ; Bower, Amy ; Furey, Heather ; Susan Lozier, M. ; Xu, Xiaobiao ( , Nature Communications)
Abstract Iceland-Scotland Overflow Water (ISOW) is a primary deep water mass exported from the Norwegian Sea into the North Atlantic as part of the global Meridional Overturning Circulation. ISOW has historically been depicted as flowing counter-clockwise in a deep boundary current around the subpolar North Atlantic, but this single-boundary-following pathway is being challenged by new Lagrangian observations and model simulations. We show here that ISOW leaves the boundary and spreads into the interior towards the central Labrador and Irminger basins after flowing through the Charlie-Gibbs Fracture Zone. We also describe a newly observed southward pathway of ISOW along the western flank of the Mid-Atlantic Ridge. The partitioning of these pathways is shown to be influenced by deep-reaching eddies and meanders of the North Atlantic Current. Our results, in tandem with previous studies, call for a revision in the historical depiction of ISOW pathways throughout the North Atlantic.
-
Susan Lozier, M. ; Bacon, Sheldon ; Bower, Amy S. ; Cunningham, Stuart A. ; Femke de Jong, M. ; de Steur, Laura ; deYoung, Brad ; Fischer, Jürgen ; Gary, Stefan F. ; Greenan, Blair J. ; et al ( , Bulletin of the American Meteorological Society)