Articles | Volume 17, issue 7
https://doi.org/10.5194/amt-17-1941-2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
Advantages of assimilating multispectral satellite retrievals of atmospheric composition: a demonstration using MOPITT carbon monoxide products
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- Final revised paper (published on 05 Apr 2024)
- Supplement to the final revised paper
- Preprint (discussion started on 23 Nov 2023)
- 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 amt-2023-238', Anonymous Referee #1, 24 Nov 2023
- AC1: 'Reply on RC1', Wenfu Tang, 24 Jan 2024
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RC2: 'Comment on amt-2023-238', Anonymous Referee #2, 15 Dec 2023
- AC2: 'Reply on RC2', Wenfu Tang, 24 Jan 2024
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Wenfu Tang on behalf of the Authors (24 Jan 2024)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (25 Jan 2024) by Meng Gao
RR by Anonymous Referee #2 (06 Feb 2024)
ED: Publish as is (14 Feb 2024) by Meng Gao
AR by Wenfu Tang on behalf of the Authors (21 Feb 2024)
Manuscript
General comments
The study conducted by Tang et al. evaluated the impact of assimilating multispectral/joint versus TIR-only retrieval, column versus profile retrieval, and joint products versus single-spectral products separately, through a 15-day inversion in CAM-chem+DART system, based on MOPITT CO database. They evaluated the assimilation performance against both the assimilated data and independent data (TROPOMI, TCCON, NOAA CCGG, IAGOS, and WE-CAN). Overall, this study is convincing and of great interest to the community studying CO or satellite retrieval, within the scope of AMT.
Readers would be benefit from understanding if such comparison remains consistent across other seasons and years. In section 7.4, the authors acknowledge that these results might not be representative for other seasons, and performing a long-term assimilation has high computational cost. Please consider a direct comparison of measurements, rather than their assimilation performance, to evaluate the potential of robustness in discrepancies and similarities across datasets over varying timeframes.
Please clarify the treatment of observation error estimates. Did the inversions include the information of observation uncertainty? Can the observation uncertainty provided by MOPITT associated with measurements, effectively highlight the useful information from each dataset?
Specific comments
Figure 3: Please explain the criteria used to reject observations too far from the ensemble mean. Providing details on the threshold or methodology employed for this rejection would enhance the transparency of the assimilation process.
Figure 5: The authors did a good job in effectively presenting the inversion performance in Figure 5, but did not discuss the 200 hPa results in the main text.
Figure 9: The two assimilations with profile observations exhibit >1 line fit. Does this indicate assimilations with profile measurements tend to overestimate emissions or surface concentration?
Line 175: Please clarify the approach to project MOPITT CO AK and prior to the model resolution.
Line 195 and 196: the order of case 1 and 2 are opposite in the text and Figure 2.
Line 211: Did the authors consider a spin-down timeframe? For observations after the assimilation timeframe while can still reflect emission signals?
Line 320: Please clarify the definition of observation error variance, and if such error estimates have been incorporated into the assimilation system.
Line 331: Please clarify the meaning of x in eq 4.
Line 351: Experiment 2 and 5 are expected to assimilate similar information, with the major difference at 200 hPa, as indicated in Figure 5.
Line 420: The mean bias in text is 0.7 ppb, while 5.72 in Figure 9. The correlation is 0.65 in text, while 0.79 in Figure 9.
Line 465: Given the assimilation timeframe is 15 days, please clarify the approach to estimate annual emissions.
Section 7.4 How about temporal resolution? Can MOPITT optimize emissions up to daily scale based on the experiments here?
Technical corrections
Table 1: Missing the labels of TEMPO spectral ranges and potential chemical species for geostationary satellites.
Line 130: typo, an extra “;” after “CAM-chem”.