the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Major sources of North Atlantic Deep Water in the subpolar North Atlantic from Lagrangian analyses in a high–resolution ocean model
Abstract. North Atlantic Deep Water (NADW) is a crucial component of the Atlantic Meridional Overturning Circulation and, therefore, is an important factor of the climate system. In order to estimate the mean relative contributions, sources and pathways of the three different deep water mass components (namely Labrador Sea Water, Northeast Atlantic Deep Water and Denmark Strait Overflow Water) at the southern exit of the Labrador Sea, Lagrangian particle experiments were performed. The particles were seeded according to the strength of the velocity field along the 53° N section and computed 40 years backward in time in the three-dimensional velocity and hydrography field. Water masses were defined within the model output in the central Labrador Sea and the subpolar North Atlantic. The resulting transport pathways, their sources and corresponding transit time scales were inferred. Our experiments show that the majority of NADW passing 53° N is associated with diapycnal mass flux, accounting for 14.3 Sv (48 %), where 6.2 Sv originate from the Labrador Sea, compared to 4.7 Sv from the Irminger Sea. The second largest contribution originates from the mixed layer with 7.2 Sv (24 %), where the Labrador Sea contribution (5.9 Sv) dominates over the Irminger Sea contribution (1.0 Sv). Another 5.7 Sv (19 %) of NADW cross the Greenland–Scotland Ridge within the NADW density class, where about 2/3 pass Denmark Strait, while 1/3 cross the Iceland Scotland Ridge. The NADW exported at 53° N is hence dominated by entrainment through diapycnal mass flux and the mixed layer origin in the Labrador Sea.
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Notice on discussion status
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
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Preprint
(19801 KB)
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(19801 KB) - Metadata XML
- BibTeX
- EndNote
- Final revised paper
Journal article(s) based on this preprint
Interactive discussion
Status: closed
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RC1: 'Review of Fröhle et al. "Major sources of North Atlantic Deep Water in the subpolar North Atlantic from Lagrangian analyses in a high–resolution ocean model"', Anonymous Referee #1, 13 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-313/egusphere-2022-313-RC1-supplement.pdf
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AC1: 'Reply on RC1', Patricia Handmann, 14 Jul 2022
We want to thank Reviewer #1 for the thorough review of our submitted manuscript. The major topics mentioned by both reviewers were in some parts similar and helped to improve our manuscript. Please find the detailed response to your review in the uploaded pdf. We answered to every point raised by the reviewer seperately in the pdf. We appreciate the constructive comments and questions raised.
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AC1: 'Reply on RC1', Patricia Handmann, 14 Jul 2022
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RC2: 'Comment on egusphere-2022-313', Anonymous Referee #2, 18 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-313/egusphere-2022-313-RC2-supplement.pdf
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AC2: 'Reply on RC2', Patricia Handmann, 14 Jul 2022
We thoroughly thank Reviewer #2 for the review of our submitted manuscript. The major topics mentioned by both reviewers were in some parts similar and helped to improve our manuscript. We answered to every point raised by the reviewer seperately in the pdf. Please find the detailed response to your review in the uploaded pdf. We appreciate the constructive comments and questions raised.
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AC2: 'Reply on RC2', Patricia Handmann, 14 Jul 2022
Interactive discussion
Status: closed
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RC1: 'Review of Fröhle et al. "Major sources of North Atlantic Deep Water in the subpolar North Atlantic from Lagrangian analyses in a high–resolution ocean model"', Anonymous Referee #1, 13 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-313/egusphere-2022-313-RC1-supplement.pdf
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AC1: 'Reply on RC1', Patricia Handmann, 14 Jul 2022
We want to thank Reviewer #1 for the thorough review of our submitted manuscript. The major topics mentioned by both reviewers were in some parts similar and helped to improve our manuscript. Please find the detailed response to your review in the uploaded pdf. We answered to every point raised by the reviewer seperately in the pdf. We appreciate the constructive comments and questions raised.
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AC1: 'Reply on RC1', Patricia Handmann, 14 Jul 2022
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RC2: 'Comment on egusphere-2022-313', Anonymous Referee #2, 18 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-313/egusphere-2022-313-RC2-supplement.pdf
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AC2: 'Reply on RC2', Patricia Handmann, 14 Jul 2022
We thoroughly thank Reviewer #2 for the review of our submitted manuscript. The major topics mentioned by both reviewers were in some parts similar and helped to improve our manuscript. We answered to every point raised by the reviewer seperately in the pdf. Please find the detailed response to your review in the uploaded pdf. We appreciate the constructive comments and questions raised.
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AC2: 'Reply on RC2', Patricia Handmann, 14 Jul 2022
Peer review completion
Journal article(s) based on this preprint
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Arne Biastoch
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(19801 KB) - Metadata XML