Articles | Volume 15, issue 11
https://doi.org/10.5194/essd-15-5079-2023
© Author(s) 2023. This work is distributed under the Creative Commons Attribution 4.0 License.
High-resolution aerosol data from the top 3.8 kyr of the East Greenland Ice coring Project (EGRIP) ice core
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- Final revised paper (published on 17 Nov 2023)
- Preprint (discussion started on 06 Jun 2023)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on essd-2023-176', Anonymous Referee #1, 03 Jul 2023
- AC1: 'Author comment for essd-2023-176', Tobias Erhardt, 29 Aug 2023
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RC2: 'Comment on essd-2023-176', Anonymous Referee #2, 05 Jul 2023
- AC1: 'Author comment for essd-2023-176', Tobias Erhardt, 29 Aug 2023
- AC1: 'Author comment for essd-2023-176', Tobias Erhardt, 29 Aug 2023
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Tobias Erhardt on behalf of the Authors (29 Aug 2023)
Author's response
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ED: Publish as is (11 Sep 2023) by Xingchen (Tony) Wang
AR by Tobias Erhardt on behalf of the Authors (05 Oct 2023)
Manuscript
This paper describes a dataset, deposited at Pangaea, that contains high-resolution (1 mm) CFA data for ions (and conductivity) from EGRIP. The data extend to 3800 years (479 m); they have been used to develop an age model so far; they are clearly supporting data for that and therefore have value, as well as future value for assessing changes in environmental factors over this time period. Much of the paper itself is devoted to describing methodology. This includes more general methodology about the drilling and CFA campaign (which also generated other data not shown here). The main novelty in the methodology compared to previous data papers concerns the ICP-TOFMS. The methodology seems clear and the data are undoubtedly of high quality, so the paper seems very publishable. I note that this is only about half the data that were measured in 2018 and 2019. While I understand why the data are being released in increments, it will be annoying for users if they remain in separate files, so I suggest that future releases are added to existing files rather than listed as separate files that readers have to splice together.
With a few minor corrections and suggestions below, I am happy to recommend publication of this data paper.
Lines 43, 51: accumulation rates are in cm/a – is this water equivalent or ice equivalent?
Fig 2 caption. Sorry to be fussy but the correct abbreviation is mL not ml. Similarly uL later.
Line 83 “samples at 5−−2.5 cm depth” – please explain what you mean by this. Do you mean “between 2.5 and 5 cm”? It’s not obvious.
Lines 84, 86, “aliquots” spelling
Line 113 “Note, that the air is released from the ice during melting and thus does not pose a contamination risk”. I’m not sure what this means, why would the air pose a contamination risk?
Fig 3, line 4 of caption “most”
Fig 3 – for comparison purposes it would be better if the y-scaling of the two Ca datasets was the same, which seems not to be the case at present.
Line 202 “mis-measurement” spelling
Section 5.2 and Fig 5. I found this section hard to follow. Please spell out what you mean by “encoder deviation” in 5G – it seems from the text as if it should be telling me about the “total discrepancy between the length of ice as measured by the encoder to the length of ice measured using sample preparation” but I don’t understand what you mean by this “encoder deviation”. Also if its 1% (typically) for a 3 m piece, how is the depth precise to 1 cm? I believe you that it is, but I’m not clear how I get that from Figure 5. The figure is also not well-designed if you aim to show that run length doesn’t affect the depth precision, as it is impossible to follow the few shorter runs down to section G.
Line 239. Figure 7 is called before Figure 6. You may want to renumber them?
Line 241 “deposition” spelling
Line 244 “88CE, corresponding to 1910 yr b2k” – am I missing something? Surely 88CE is 1912 b2k?
Line 303 “Here we…”