Articles | Volume 18, issue 10
https://doi.org/10.5194/essd-18-7475-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
High-quality remote sensing reflectance products over China and US coast
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- Final revised paper (published on 13 Oct 2026)
- Preprint (discussion started on 13 Aug 2025)
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 essd-2025-438', Anonymous Referee #1, 19 Sep 2025
- AC2: 'Reply on RC1', Shuhui Zhao, 28 Feb 2026
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RC2: 'Comment on essd-2025-438', Anonymous Referee #2, 19 Dec 2025
- AC1: 'Reply on RC2', Shuhui Zhao, 28 Feb 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Shuhui Zhao on behalf of the Authors (28 Feb 2026)
Author's response
Author's tracked changes
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ED: Referee Nomination & Report Request started (04 Mar 2026) by François G. Schmitt
ED: Publish as is (17 Sep 2026) by François G. Schmitt
AR by Shuhui Zhao on behalf of the Authors (21 Sep 2026)
The manuscript aims to construct a high-quality Rrs dataset covering coastal waters of both China and the United States. An AC processing framework that integrates standard NIR-based AC and grided aerosol model AC were developed. Moreover, cloud masking constraint was relaxed to get more effective data. While the topic is important as Rrs products in coastal areas is still have relatively high uncertainty as compared to it in open oceans, the high quality promoted by the title does not match the actual results for the following four major reasons.
1. Relaxing cloud masking constraint of course would enlarge effective data portion, but it would degrade data quality or accuracy of the Rrs products especially in clear waters. Therefore, this contradicts the goal of obtaining high-quality Rrs dataset.
2. The representativeness of grided aerosol models in instantaneous satellite images of coastal or shelf waters is questionable. This issue includes two parts. One is the temporal representativeness, since the grided aerosol models are multi-years and monthly averaged data, it can’t represent the instantaneous aerosol conditions. For example, even for some coastal oceans that are often affected by absorbing aerosols, the aerosol type may still be non or weak-absorbing aerosols in a specific day's image. In this case, if the average absorbing aerosol is still used, the accuracy may decrease. Another one is the spatial representativeness, aerosol types are high spatial heterogeneity, the large grid size (5 degree) makes it difficult to ensure that the grided aerosol models can represent the real aerosol types of each pixel, especially for grids with only one AERONET station far from the coastline.
3. There is no scientific basis for using water turbidity to distinguish between grided aerosol models and traditional AF10 aerosol models. The regulation mechanisms of water turbidity and aerosols are different, and there is no necessary connection between the two.
4. The standard NIR AC algorithm has a high degree of uncertainty in turbid water, which has been widely recognized. Therefore, comparing the results with NIR AC algorithm in this study cannot fully demonstrate the superiority of the proposed method. It is recommended to compare it with existing atmospheric correction results for turbid water, such as OC-SMART, POLYMER, NIR-SWIR, etc.