Articles | Volume 17, issue 2
https://doi.org/10.5194/amt-17-453-2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
Special issue:
First results of cloud retrieval from the Geostationary Environmental Monitoring Spectrometer
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- Final revised paper (published on 24 Jan 2024)
- Preprint (discussion started on 10 May 2023)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on amt-2023-91', Anonymous Referee #1, 14 Jun 2023
- AC1: 'Reply on RC1', Bo-Ram Kim, 03 Aug 2023
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RC2: 'Comment on amt-2023-91', Anonymous Referee #2, 28 Jun 2023
- AC2: 'Reply on RC2', Bo-Ram Kim, 03 Aug 2023
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Bo-Ram Kim on behalf of the Authors (07 Aug 2023)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (22 Aug 2023) by Rokjin Park
RR by Anonymous Referee #1 (07 Sep 2023)
RR by Anonymous Referee #2 (23 Sep 2023)
ED: Reconsider after major revisions (25 Sep 2023) by Rokjin Park
AR by Bo-Ram Kim on behalf of the Authors (27 Nov 2023)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (01 Dec 2023) by Rokjin Park
AR by Bo-Ram Kim on behalf of the Authors (02 Dec 2023)
Manuscript
This manuscript explained and summarized the developed algorithm of the cloud for GEMS. It is a noble paper for the report on the GEMS operational algorithm. Because of this reason, it is suitable to publish this special issue.
However, several improvements are required for the confidence of retrieval algorithm results during the revision process.
1) To improve the structure of this paper, it is necessary to revise the order of sections.
Especially, Sections 2.2 and 3.1 are too similar. Please merge the two sections into one section.
2) To explain the GEMS radiance characteristics, sampling and resolution information are wrong. The sampling is 0.2 nm and the resolution is 0.6 nm. Please correct it.
3) Section 2.2 has to be moved before Section 2.1. Algorithm outputs are more appropriate after the algorithm description.
4) L139: For the radiance simulation, this study used 460-485 nm. However, the O2-O2 band at 477 nm significantly affect the spectral range longer than 485 nm. Why does this study use the spectral range with not wide enough?
5) L144: This spectral range is significantly affected the NO2 absorption. Why does this study not consider the NO2 absorption?
6) L156: From Equation (3), this equation is not a full DOAS method. It is linearized absorption signal separation. The full DOAS method is additionally considered the non-linear correction. How about correcting the non-linear effect for the estimation of SCD?
7) L161: For readability, please add the flowchart of the whole cloud retrieval algorithm.
8) L162-L166: It is too simple to explain. Please add the details of the explanation what is the main difference between the two different platforms.
9) Section 3.1 (before revision): This section needs to separate the sections according to the platforms.
10) L248: This manuscript is only focused on the Korean Peninsula, not the GEMS domain. Do you have some reasons? Please clarify this issue.
11) Section 4: This manuscript is focused on the cloud algorithm for GEMS. However, Section 4 shows the results using OMI and TROPOMI. Please clarify the purpose of these results.
12) Figure 3: This figure is one of the key results in this manuscript. However, as shown in this figure, an arbitral stripe pattern exists. I think that this is a problem during the inversion process for the best solution estimation from LUT. This problem is a critical issue for the operational algorithm. Please check and find the reason and need to fix this critical issue.
13) Section 5: Although the manuscript shows several cases, the long-term comparison result is also required to see the stability of the algorithm's accuracy. In addition, this study only showed the 0430 UTC result. It is only allowed to the intercomparison. To see the diurnal variability of cloud retrieval results, this study also has to show the continuous diurnal results. In addition, some performance results (statistical validation results) are essential.
Minor Comment
1) L160: angle geometry --> observation geometry
2) L168: Please add the reference for the VLIDORT NGST version.
3) L199: Please add the reference, and recheck the spatial resolution of TROPOMI in L204.
4) L241: To the clarify the difference, please list-up the difference of definition for cloud parameters.
5) L285-286: This sentence is not clear. Please rephrase it.