Articles | Volume 19, issue 11
https://doi.org/10.5194/gmd-19-4775-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
A unified Hapke-HSR + MARMIT-2 soil radiative transfer model for reflectance simulation under varying moisture conditions
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- Final revised paper (published on 03 Jun 2026)
- Preprint (discussion started on 03 Mar 2026)
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 egusphere-2026-344', Anonymous Referee #1, 27 Mar 2026
- AC1: 'Reply on RC1', Anxin Ding, 23 Apr 2026
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RC2: 'Comment on egusphere-2026-344', Anonymous Referee #2, 10 Apr 2026
- AC2: 'Reply on RC2', Anxin Ding, 23 Apr 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Anxin Ding on behalf of the Authors (30 Apr 2026)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (09 May 2026) by Cenlin He
RR by Anonymous Referee #2 (11 May 2026)
ED: Publish as is (24 May 2026) by Cenlin He
AR by Anxin Ding on behalf of the Authors (26 May 2026)
Manuscript
The manuscript proposes a coupled soil radiative transfer model by integrating the improved Hapke-HSR model with the MARMIT-2 model to simulate soil spectral reflectance under varying moisture conditions. The topic is relevant, and the study demonstrates promising results across multiple datasets. The manuscript shows clear novelty, with a well-organized structure and generally good writing quality. I recommend publication after major revisions. I encourage the authors to address the following comments.
1. Although the proposed coupled model shows promising performance, the novelty of the study could be further clarified. It is recommended to explicitly highlight the key innovations of the proposed approach in comparison with existing models (e.g., Hapke or MARMIT-2) in the Introduction, to strengthen the overall contribution of the manuscript.
2. Several models are listed in Table 1; however, it is not entirely clear why the Hapke-HSR and MARMIT-2 models were selected for coupling instead of other possible combinations (e.g., BSM with Hapke-HSR). A brief justification for this choice would improve the clarity of the study design.
3. The manuscript should provide clearer references or methodological explanations regarding how the optimal values of parameters such as B0, h, b′, c, and c′ are determined. In addition, since both b and c influence the BRDF shape in the Hapke model, it would be helpful to clarify why the discussion primarily focuses on parameter b.
4. In the current manuscript, the distinction between input parameters and retrieved parameters is not always clear, particularly in some tables. It is recommended to clearly differentiate these parameter types and ensure consistent terminology throughout the manuscript.
5. The study is mainly conducted under a fixed observation geometry. It would be beneficial to further discuss how this assumption may influence the model results, as well as the applicability of the model under different viewing and illumination conditions.
6. Although the validation results are generally convincing, the study could be further strengthened by including comparisons with additional models (e.g., GSV or similar approaches), or by providing more discussion on the differences between the proposed model and existing methods.
7. The coupling strategy between the improved Hapke-HSR model and the MARMIT-2 model is not entirely clear. It would be useful to clarify whether the parameters (b, M, δ, L, ε) are retrieved sequentially or simultaneously, and to provide a clearer description of the integration workflow.
8. In the Discussion, the manuscript attributes the decrease in model accuracy (when using averaged χsoil) mainly to differences in soil types. However, soil properties (e.g., organic carbon content, texture) can vary significantly even within the same soil type and may strongly affect spectral absorption. It is suggested to consider incorporating soil property variability or grouping spectrally similar soils when defining χsoil, which may further improve model performance.