Articles | Volume 23, issue 6
https://doi.org/10.5194/bg-23-2079-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Interpreting carbon-water trade-offs in Daisy crop model using Pareto-based calibration
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- Final revised paper (published on 26 Mar 2026)
- Preprint (discussion started on 27 Nov 2025)
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-2025-4987', Anonymous Referee #1, 12 Jan 2026
- AC3: 'Reply on RC1', Laura Delhez, 12 Feb 2026
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RC2: 'Comment on egusphere-2025-4987', Anonymous Referee #2, 21 Jan 2026
- AC1: 'Reply on RC2', Laura Delhez, 12 Feb 2026
- AC2: 'Reply on RC2', Laura Delhez, 12 Feb 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (16 Feb 2026) by Anja Rammig
AR by Laura Delhez on behalf of the Authors (11 Mar 2026)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (12 Mar 2026) by Anja Rammig
RR by Anonymous Referee #2 (15 Mar 2026)
ED: Publish as is (16 Mar 2026) by Anja Rammig
AR by Laura Delhez on behalf of the Authors (17 Mar 2026)
Manuscript
General comments
The paper clearly demonstrates the challenges of simulating the links between stomatal opening, dry matter production, and the fluxes of water and CO₂ using an advanced soil–water–plant–atmosphere model with a fully coupled photosynthesis and energy balance scheme for simulating plant transpiration. The work is extensive and builds upon a comprehensive sensitivity analysis of 200 parameters to identify the most influential ones. In the present study, these parameters are calibrated using a Pareto-based calibration strategy and high-quality eddy covariance data from four growing seasons. Overall, the work is well structured and appears to be of high quality. In general, I have some comments, mostly suggestions related to the discussion on specific parts of the manuscript, as outlined below.
In my opinion, the main limitation of the study is the lack of data on soil water dynamics in different soil layers. It would have been very informative to evaluate how well the model simulated soil drying, both due to root water uptake and soil evaporation. Although different combinations of soil physical properties were tested in the sensitivity analysis and some root parameters were calibrated, the selected parameter set may not have been optimal. Such data could also have helped to identify the causes of the discrepancies between simulated and observed evapotranspiration. This aspect is missing from the discussion. A similar issue applies to the lack of leaf area data, which is only represented indirectly through biomass measurements of the different plant organs.
Specific comments
It would be relevant to mention the work of Delhez et al. (2025) already in the introduction. Currently, this study is cited only in the Materials and Methods section as the source of data, management and soil information, and the internal sensitivity analysis. However, it may be useful to clarify that the present study is a follow-up to that work, focusing on the calibration of the most relevant parameters identified previously. This could be stated in the final part of the introduction.
Line 55:
It could be useful to explain why Daisy was selected for this study compared to the other models mentioned earlier (lines 25–30). It is unclear whether Daisy is unique in coupling Richards’ equation for soil water dynamics with a Farquhar-based photosynthesis model, or whether the choice was driven by other factors. For example, Daisy being open source and implemented in C++ may have facilitated the implementation of the Pareto-based modelling framework.
Lines 90–95:
Is the Daisy setup similar to that used in Delhez et al. (2025)? If so, it may be relevant to mention that a drainage system based on the Hooghoudt equation is included. Alternatively, this information could simply be referenced to Delhez et al. (2025), where it is described. Otherwise, there is a risk of soil profile flooding when an aquitard layer is present and no drainage system is implemented.
Figure 5. A latent heat flux of 600 w/m2 in late April seems extreme, since the theoretical potential clear sky radiation is 750 w/m2. Would have been relevant to see the data on air temperature, humidity, and wind speed during this event.
Section 4.2:
The issue of calibrating the model separately for each cultivar grown in only one season is not discussed. For instance, the large differences observed in some parameters may be difficult to explain purely on a genetic basis. The large range in parameters such as SOrgPhotEff and stemPhotEff could potentially be caused by seasonal stress factors—such as disease or water or nitrogen stress—not explicitly represented in the model, rather than by genetic differences. It might have been more robust to calibrate a single cultivar across all seasons, given that modern wheat cultivars generally do not differ substantially in yield potential or growth patterns.
Lines 330–340:
It could be added that models based on Richards’ equation tend to overestimate soil evaporation. One reason is the difficulty in obtaining accurate hydraulic parameters for the surface soil layers, which is further complicated by soil water hysteresis. As a result, the hydraulic conductivity curve used to calculate potential matrix exfiltration may be too high, leading to an overestimation of soil evaporation in Daisy. This issue will also be relevant for a model with a more mechanistic coupling between the surface energy and water balance, simulating microclimate effects on soil EP as a fully coupled approach.
Lines 330–340 (continued):
Daisy also includes a transfer function controlled by the EpInterchange coefficient, which allows energy transfer from a dry soil surface to the canopy (default value β = 0.6 [–]). This function could potentially explain the relatively high simulated latent heat flux (LE) during periods of low leaf area at the beginning and end of the time series. In theory, this parameter could convert some soil water into LE under dry surface conditions. The parameter was not included among the 200 parameters in the initial sensitivity analysis by Delhez et al. (2025), and its omission may have resulted in an overestimation of transpiration as a starting point for the SSOC iterations.
Again, this interpretation assumes that Daisy uses accurate hydraulic conductivity curves for the surface layers, as discussed above.
Technical corrections
Line 70:
The following sentence is confusing: “(Meza et al., 2018; 2023). As the same cultivar was sown for VAL and SAH, the VAL season was set aside for validation.” This is unclear. Instead of naming growing seasons after cultivars, it might be clearer to refer to them by year. Furthermore, as noted above, it is not clearly stated whether a specific calibration was performed for each cultivar/season or whether a single parameterised cultivar was used across all seasons in the text. This information is only apparent from Table B1 in Appendix B.
Table 2:
Not all parameters listed can be found in the Daisy documentation. For example, it is unclear what k_net refers to in the Daisy reference manual. It would be helpful to include the exact name from the setup files in this list as a separate column.