the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 17 Sep 2025
The Arctic overturning circulation: transformations, pathways and timescales
Abstract. The Arctic is the northernmost terminus of the Atlantic Meridional Overturning Circulation and is an important source of the densest waters feeding its lower limb. However, relatively little is known about the structure and timescales of the Arctic overturning circulation, and which pathways contribute most to the transformation of Atlantic Waters into dense waters and Polar Waters. In this work, we combine a Eulerian water mass transformation framework and Lagrangian tracking to decompose the time-mean Arctic overturning circulation in an eddy-rich (1/12˚) global ocean hindcast (1979–2015). We show that the Atlantic Water branch through the Barents Sea dominates dense Arctic overturning, and that a large portion of these transformed waters takes many decades to exit Fram Strait. Furthermore, we show that surface forcing in the Barents Sea and north of Svalbard dominates dense overturning, but local subsurface mixing with shelf waters and between the two Atlantic Water branches plays an important role for the Fram Strait branch. Our work identifies the dominant processes of the Arctic overturning circulation, and contributes to understanding its future changes and their impact on the stability of northern overturning.
- Preprint
(17310 KB) - Metadata XML
- BibTeX
- EndNote
Status: final response (author comments only)
- RC1: 'Comment on egusphere-2025-4345', Anonymous Referee #1, 26 Sep 2025
-
RC2: 'Comment on egusphere-2025-4345', Anonymous Referee #2, 06 Nov 2025
Overall comments:
This is an interesting and useful paper on Arctic Ocean overturning circulation. I agree with the authors that “it is important to understand how Atlantic Water entering the Arctic Ocean is transformed” (line 46) and that the “the relative contributions of surface forcing and interior mixing are not” known (line 48), or “where along the Atlantic Water pathways the transformation is most pronounced”. These are all good topics to study that are relevant to the readers of Ocean Science. The methods are appropriate, well-described, and well-executed and the results are well supported. The conclusions are useful for oceanographers studying the Arctic overturning circulation and water mass transformation.
The paper is clear, well-organized, accurate, and well-written with an appropriate title and abstract. With a few important caveats (see below), the paper is novel and well situated in the literature on Arctic Ocean overturning.
In terms of scientific significance, the paper rates as Good.
In terms of scientific quality, the paper rates as Good.
In terms of presentation quality, the paper rates as Excellent.
I have three related major suggestions on connecting the present paper with prior studies, and several minor suggestions. I recommend the paper is returned to the authors for a major revision then reconsidered for publication by Ocean Science.
Specific major comments:
The present paper should carefully consider a closely related paper on Arctic Ocean water mass transformation by Pemberton et al. (2015, JPO, 10.1175/JPO-D-14-0197.1, it’s not cited in the present paper). It's important to compare and contrast the present results with those in this earlier paper. For instance, Figures 4, 5, and 11 of the present paper show the same quantities as various Figures in Pemberton’s paper. Of course, there are important differences between the two studies, like the refined model resolution and spatial information in the present paper. A careful discussion to compare and contrast the two studies is needed. For instance, Pemberton et al. discuss the importance of their surface salinity restoring on their estimates of water mass transformation (it’s not negligible, e.g., see their conclusion). The present model also includes surface salinity restoring, and fixing this unrealistic aspect of the model configuration is an important next step.
Also, the present paper should discuss the results of Tsubouchi et al. (2024, which is cited in the present paper) in more depth. For instance, Figures 4 and 6 of the present paper show the same quantities as Figure 4 of Tsubouchi et al. (2024). Again, there are important methodological differences, but a careful discussion is needed. For instance, the overturning in density space shown in Figure 4 of the present paper has a significantly different split between the Barents Sea and Fram Strait compared to Tsubouchi’s paper (see line 252). Because Tsubouchi et al.’s estimates are (mainly) based on observations at gateway sections, they don’t suffer from the surface-salinity-restoring issue mentioned above (although they have other issues, of course). Some discussion of the possible reasons for the differences, and therefore, the pros and cons of each study, would be helpful.
Finally, the present paper should discuss the new study by Brown et al. (2025, AGU Advances, 10.1029/2024AV001529, it’s not cited in the present paper). Brown et al. update and extend the Tsubouchi et al. (2024) paper. Brown et al.’s results represent the current best estimate of Arctic water mass transformation from gateway observations and surface flux reanalyses. The present paper should compare and contrast its results with their study, and carefully discuss the reasons for the differences and the pros and cons of each approach.
Specific minor comments:
Abstract: The last sentence mentions how this paper “contributes to understanding…future changes” in the Arctic overturning circulation. This is mentioned again in the final sentence of the main text (lines 415–416), where it talks about establishing a baseline of Arctic overturning. This is all fine, but the abstract had me expecting something more involved, so I suggest you mention “baseline” in the final sentence of the abstract too.
Line 73: Describing Beszczynska-Moller et al’s 2012 paper as “recent” stretches the definition of “recent" a bit.
Line 95: The final two terms seem inconsistent with equation 5. Should they be the derivatives of G_\Theta and G_S (not G_{S \Theta}? If not, how is G_{S \Theta} connected to G_\Theta and G_S?
Line 120: It talks about the residuals including “sea-surface restoring”. Remind the reader here that this model has surface salinity restoring (line 63) that will appear in the residual term.
Line 155: Is the “long term trend of buoyancy gain in the Arctic Ocean deep waters” a real physical signal? Or is it model drift? (Or something else?).
Line 215: It talks about the formation of the densest waters in the Arctic (saline, freezing Barents Sea water). State the density, salinity and temperature of these waters in the model.
Lines 264–265: Explain how the 60% and 40% numbers are found.
Figure 6b: I don’t understand how this figure is made. Please explain.
Lines 303–304: It talks about the surface transformation occurring through cooling, melting, and/or freezing. What are the relative contributions of each of these processes?
Figure 7a: I don’t understand how the “overturning in density space” is calculated. Please explain.
Lines 350–361: The method to estimate the relative contributions of surface forcing and internal mixing to water mass transformation is ad hoc. It’s hard to judge how reliable the results are, although it’s reassuring to read that numbers are robust to the threshold. How can this method be tested and improved?
Line 394: The text brushes off the apparent disagreement with the Årthun et al. (2025) paper by saying it will be a topic of another study. Meanwhile, can you speculate as to how the disagreement might be reconciled? What are the most likely explanations?
Figure A1: What’s the time period for the two datasets?
Typos etc.:
Line 101: “\nu” (I think) in the integrand should be $v$ (as on line 103).
Line 353: “criteria” should be singular (“criterion”).
Citation: https://doi.org/10.5194/egusphere-2025-4345-RC2 -
EC1: 'Comment on egusphere-2025-4345', Sjoerd Groeskamp, 14 Nov 2025
I thank the reviewers for their effort reviewing this manuscript.
Both reports provide very positive feedback on this paper and consider it worthy for publication after minor revisions and improvements are made. I therefore invite the authors to provide detailed point by point response to the reviewers comments and upload a revised version of their manuscript for consideration for publication in Ocean Sciences.
Citation: https://doi.org/10.5194/egusphere-2025-4345-EC1
Data sets
Lagrangian trajectory data in the Arctic Ocean Jakob Dörr https://doi.org/10.5281/zenodo.17047093
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 887 | 81 | 13 | 981 | 30 | 25 |
- HTML: 887
- PDF: 81
- XML: 13
- Total: 981
- BibTeX: 30
- EndNote: 25
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
Please see the attachment.