Articles | Volume 5, issue 4
https://doi.org/10.5194/wcd-5-1523-2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
A global climatology of sting-jet extratropical cyclones
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- Final revised paper (published on 17 Dec 2024)
- Supplement to the final revised paper
- Preprint (discussion started on 28 May 2024)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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- RC1: 'Comment on egusphere-2024-1413', Emmanouil Flaounas, 08 Jul 2024
- RC2: 'Comment on egusphere-2024-1413', Anonymous Referee #2, 27 Aug 2024
- AC1: 'Comment on egusphere-2024-1413', Suzanne L. Gray, 20 Sep 2024
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Suzanne L. Gray on behalf of the Authors (18 Oct 2024)
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ED: Publish subject to technical corrections (24 Oct 2024) by Lukas Papritz
AR by Suzanne L. Gray on behalf of the Authors (24 Oct 2024)
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Review of the paper "A global climatology of sting-jet extratropical cyclones" by Gray et al., 2024.
I read the paper with great interest and I found it helpful and insightful, providing a richness of interesting results. A global climatology of sting-jet cyclones was indeed missing from the state of the art and this paper provides an overview of these systems' structural characteristics and insights into their dynamics. I have comments and suggestions of minor nature on the organization of the manuscript that I leave to the authors discretion if they want to follow them.
Section 2 is clearly described, albeit complicated and long. Complexity is not due to language or presentation, but due to the large amount of knowledge and techniques that someone needs to understand and be already familiar with. Probably sections 2.1, 2.3 and 2.6 could go together. Then, sections 2.2 and 2.4 could form a separate (sub)section which could be supported with schematics or flowcharts so that the reader can conceptually understand the role of different dynamical features in sting-jets. A subsequent subsection could use real cases as examples (now figures 1 to 3) to demonstrate the complexity of the exercise and what is expected in realistic datasets. Finally, section 2.5 although it is important it could be moved to supplement or an appendix.
I am not sure there are many(any?) climatologies of warm seclusions (SJP+nSJP). It would be useful to know a bit more on how they compare spatially to other intense cyclones.
Section 3.1: If most SJP cyclones include a sting jet and if ERA5 may partly resolve these sting jets, then is it possible that sting jets are responsible for higher relative vorticity at 850 hPa in the center of the cyclones in T63 resolution? If so, then SJP cyclones should anyway be more intense than other cyclones (if we use relative vorticity as an intensity metric). A reply comes later in section 3.4, so I am wondering if this section should be merged with 3.4? (Please also see next comment on section 3.6).
Section 3.6: seems a bit weaker and detached from the rest of the paper and is only confirming that SJP cyclones inlcude higher wind speeds. I am wondering if there should be a unique subsection that discusses the intensity of the cyclones involved in this analysis (i.e. merging current sections 3.1, 3.4 and 3.6).