the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 04 Aug 2025
Quantifying the response of water and carbon balances to land cover and climate extremes across Germany
Abstract. Land cover and extreme weather events are closely connected to water yield and carbon sequestration. Understanding the tradeoffs between carbon and water and how they respond to human disturbances is critical for quantifying ecosystem services. The monthly scale ecosystem model, WaSSI, was tested and applied across Germany for mapping carbon and water balances from 2001–2019. We estimated that Germany generates 84.86 billion m3 of discharge and sequesters 106.03 Tg of carbon annually. The eastern states were comparatively drier than the rest of the country, as most of their precipitation was lost as evapotranspiration. Croplands, urban areas and Evergreen Needle Forests (ENF) provide 82.5 % of the water yield, while the forests sequester the major share of carbon (56.3 %) altogether. The results highlight the importance of sparse land covers (e.g. wetlands) in carbon sequestration. Findings also suggest that national water yield and carbon balances are sensitive to extreme events. In 2002 and 2013, due to high precipitation, the stocks of key ecosystem services were notably higher. Similarly, during the drought years of 2003 and 2018, the services were reduced drastically, but we found that buffers from the previous year played an important role in mitigating negative impacts. This study highlights that, when integrated with local data, a relatively simple modelling approach is adequate to answer questions of coupled water and carbon responses to climatic variability at a large scale. We conclude that land management of both forests and croplands are vital to sustain ecosystem services under a changing climate.
- Preprint
(3634 KB) - Metadata XML
-
Supplement
(686 KB) - BibTeX
- EndNote
Status: final response (author comments only)
-
RC1: 'Comment on egusphere-2025-1629', Anonymous Referee #1, 29 Sep 2025
-
AC2: 'Reply on RC1', Karim Pyarali, 30 Nov 2025
Thank you for taking the time to share your feedback. We truly appreciate your valuable insights and will use them to guide our improvements. We have provided responses to each of your comments (highlighted in bold and italics). At this stage, the comments have not been incorporated into the manuscript, as per the editor’s instructions to refrain from making revisions at this time.
Major comments:
- Lines 204 and 229: I recommend describing the performance of streamflow (Q) and evapotranspiration (ET) validation for the same watershed(s), as this would provide a more complete view of how the model represents the water balance. In addition, you could extend the validation analysis by describing how the model captures ET and Gross Primary Productivity (GPP) at sites where both variables are available
Response: Thank you for the helpful suggestion. In our case, the Q and ET validation datasets originate from different observation systems located in different areas: streamflow measurements are taken from gauging stations, while ET is derived from eddy‐flux towers at the site level with a spatial scale at about 1 km2. The watersheds and flux towers do not spatially overlap. Therefore, joint evaluation of Q and ET at the watershed level is not feasible with the currently available data due to scale and location mismatch.
However, ET and GPP are both observed at the same eddy‐flux tower sites, and our analysis already reflects model performance where both variables are measured concurrently. This can be confirmed by comparing the site lists in Table S5 (ET) and Table 1 (GPP). We will clarify this in the revised manuscript.
- Could you provide a potential explanation for why the model tends to overestimate ET during winter? What are the implications for your results?
Response: Thank you for this comment. A likely explanation for the winter overestimation of ET is related to the way ET is parameterised in WaSSI. The model estimates actual ET as a function of potential ET (PET), precipitation, and leaf area index (LAI). During winter, LAI is low; however, precipitation is generally high in Germany, and the model formulation (see Equation 1) imposes a positive relationship between precipitation and actual ET. As a result, the model may produce higher ET values than expected under cold-season conditions. Local corrections either the PET model (derived from the eastern U.S.) or the Equation 1 (derived from global flux data) might be needed to accurately simulate ET for winter in Germany.
- Since the analysis is focused on extreme dry–hot and wet–cold years, how does the model perform during drier years (e.g., MAP < 25th percentile) and wetter (e.g., MAP > 75th percentile) years?
Response: Thank you for this important question. The WaSSI model demonstrates strong overall validation results, indicating reliable performance for diverse environments. The model performance for dry-hot extremes (e.g., drought) has been studied in multiple studies. For example, Al-Qubati et al. (2023) showed that the WaSSI model performs well under drought conditions, effectively simulating water yield and ecosystem responses in dry years across different environmental settings. This provides confidence in the model’s behaviour during years when MAP falls below the 25th percentile. In contrast, we are not aware of studies that explicitly evaluate WaSSI performance during anomalously wet years (e.g., MAP > 75th percentile). Although WaSSI performs well in general hydrological validation, its specific performance in wet years has not been systematically tested in the existing literature. As a result, our assessment of wet-year behaviour relies primarily on the validations presented in this study.
- Figure 6: Are the simulated GPP and NEP variations (i.e., decreases and increases) consistent with observed changes from eddy covariance towers and satellite observations? This may provide a better indication of whether the model accurately captures the sensitivity of GPP and NEP to precipitation and temperature anomalies.
Response: Eddy-flux observations are available only at a limited number of point locations, and aggregating these sparse measurements to a national scale would introduce substantial uncertainty and would not provide a reliable basis for evaluation. Regarding satellite products, we have already incorporated them in our validation, which provides a reasonable model performance. For these reasons, we believe that the current validation framework sufficiently supports the model’s ability to capture key ecosystem carbon dynamics. Lastly, a trend analysis was out of the scope of this study.
- I recommend adding the model parameterisation to the supplementary material, as this would make the study easier to reproduce.
Response: Thank you for this suggestion. The parameterisation of the WaSSI model for Germany followed the workflow described in Al-Qubati et al. (2023), where we tested multiple input datasets (e.g., ET formulations, snowmelt parameters, land-cover and soil datasets) and selected the combinations that yielded the best performance. In the current manuscript, we already provide the final parameter sets and input datasets used in the simulations
- Line 277: I suggest conducting the analysis while accounting for the area of each land cover type. The high-water supply attributed to croplands may largely reflect their dominant extent in Germany. Similarly, the ecohydrological role of forests could be underestimated due to their smaller extent in the country. I encourage authors to present the results considering the mean and variability contribution of each land cover (mean ± SD m3 ha-1 yr-1). This approach would also allow you to discuss the potential implications of land-cover change (e.g., forest to cropland) on the provision of ecosystem services.
Response: Thank you for this insightful suggestion. For carbon sequestration, our results are already reported on a per-area basis (per m²) for each land-cover type. For water supply, however, our current results are expressed as total values aggregated by land-cover type. We agree that presenting water-supply estimates by area would provide a clearer understanding of the contribution of each land cover
- Lines 264 and 289: The definition of drought and flood events typically incorporates not only precipitation anomalies but also temperature, along with other indicators such as soil moisture or vapour pressure deficit. Additionally, since both precipitation and temperature are inputs into the WaSSI model, I suggest that you characterize both precipitation and temperature anomalies, including temperature anomaly maps in your analysis (e.g., Figs. 8 and 9). In addition, while droughts often extend over large areas, flood-affected regions are more likely to be concentrated along river channels and flat terrains, whereas your analysis is at the country scale. Therefore, the terms ‘hot-dry’ and ‘wet-cold’ years may provide a clearer description of the extreme climate events.
Response: We will incorporate temperature anomalies into the analysis and add them in Figures 8 and 9. We also appreciate the point regarding terminology. We will adopt the terms ‘hot–dry’ and ‘wet–cold’ years to more accurately describe the climatic extremes analysed in this study. These changes will be reflected in the revised manuscript.
- Lines 314-396: You provide a lot of valuable insights in the discussion section. However, you should consider focusing more clearly on the three main results of the manuscript (i) model validation, including comparisons with previous studies; (ii) water yield and carbon sequestration associated with each land cover and the land cover change implications; and (iii) the response of these ecosystem services to extreme climatic conditions, including comparisons with previous studies and their implications under future climate projections in Germany.
Response: Thank you for this helpful suggestion. We agree that the discussion would benefit from a clearer emphasis on the three main components of the study. The current version already includes substantial discussion of the model validation and the responses of ecosystem services to extreme climatic conditions, and we will ensure that these sections are more explicitly linked to our key findings and to relevant previous studies.
Regarding the second point, we will expand the discussion on water yield and carbon sequestration associated with each land-cover type and clarify the implications of land-cover differences for ecosystem service provision. This additional synthesis will improve the structure and focus of the discussion. These revisions will be incorporated in the updated manuscript.
Minor comments:
- Line 15: Please add the full name of the WaSSI model
Response: Thank you for highlighting these points. We will take care of it in the revised manuscript.
- Line 16: I suggest replacing “from 2001-2019” with “from 2001 to 2019”
Response: Thank you for highlighting these points. We will take care of it in the revised manuscript.
- Line 52: Add space
Response: Thank you for highlighting these points. We will address this in the revised manuscript.
- Lines 85-88: I suggest adding a paragraph in the introduction to describe the generality of the model, particularly its previous applications.
Response: We agree with this point. We will address this in the revised manuscript.
- Line 109: Please add the corresponding reference(s) to the eddy flux dataset.
Response: Sure, will be done in the revised manuscript
- Lines 115-116: Please specify if, at the monthly scale, the correlation between GPP and ET is linear or not.
Response: According to Sun et al. (2011), the relationship of monthly GPP with ET was estimated using linear regression procedures (SAS v9.1.3, Cary, NC). We will explicitly state this the revised manuscript.
Sun et al. (2011) : https://doi.org/10.1029/2010JG001573
- Line 119: I am particularly familiar with the WaSSI model, but I am curious if this includes any calibration process.
Response: Yes, a calibration process was conducted prior to applying the WaSSI model in Germany. Specifically, we evaluated the performance of multiple evapotranspiration (ET) formulations, tested alternative snowmelt parameter settings, and compared different land-cover and soil datasets. The combination of parameters and input datasets that produced the best model performance was then selected and independently validated.
- Line 124: Is R2 the coefficient of determination? Please specify.
Response: Yes, R2 refers to the coefficient of determination. We will clarify this explicitly in the revised manuscript
- Line 125: Which MODIS product? Add the corresponding reference.
Response: It is the MODIS ET product MOD16A2GF. This information is provided later in the section of the Dataset. We will insert the corresponding reference in the revised Manuscript.
- Line 126: Please clarify why you computed the monthly deviations and describe the interpolation process, as this is not clear in the methodology.
Response: We computed monthly deviations because WaSSI produces output at a monthly temporal resolution, and most of our validation was also performed at the monthly scale (with the exception of Tables S4, S5, and S6, which present annual values). Therefore, no temporal interpolation or downscaling was required. Monthly values were simply aggregated to annual totals when annual comparisons were needed. We will rephrase lines 124–127 in the revised manuscript to clarify this more clearly.
- Line 127: Which MODIS product? Add the corresponding reference to the MODIS and CGLS products.
Response: It is the MODIS GPP product MOD17A2HGF. This information is provided later in the section of the Dataset. We will insert the corresponding references in the revised Manuscript.
- Line 129: Please add the description of the extent of the included watersheds for Q validation
Response: Could you please clarify what you mean by ‘extent’? A similar point was raised by Reviewer #1, and in the revised manuscript we will clarify that the chosen upstream stations were selected to ensure spatial coverage across Germany, representing the country’s major climatic zones, land use, and land cover types. We also prioritised stations with long and continuous discharge records.
- Line 160: What is meant by anthropogenic influence? Does this refer to dams, land cover change, or other factors?
Response: Yes, in this context, anthropogenic influence refers to human infrastructure or activities that modify the natural flow regime of rivers. This includes dams and reservoirs.
- Line 191: I suggest presenting the results of the main figures first (e.g., Figure 2) and then supporting your analysis with supplementary Figures and tables.
Response: Sure, will be done in the revised manuscript
- Figure 2: Add the performance metrics in each panel. All you can order the panels following a criterion such as watershed area, natural/transformed land cover area, or annual precipitation
Response: We can add the performance metrics to each panel in Figure 2 and will include them in the revised version. However, reordering the panels based on watershed area, land-cover characteristics, or annual precipitation would require additional processing steps and resources that are beyond the scope of the current revision.
- Line 199: I am curious if the model exhibits any dependence on watershed area or dominant land cover types regarding its performance?
Response: In our analysis, we did not observe any clear dependence of model performance on watershed area or land cover within Germany
- Line 205: I think this corresponds to the methods section.
Response: We will revise it in the manuscript
- Figure 3: Please add performance metrics. Please clarify in the scatterplot labels and lines legend which correspond to observations and simulations.
Response: We will add the performance metrics to Figure 3 in the revised manuscript. As noted in the figure caption, the simulated values are labeled with the corresponding WS_ID.
- Line 224: I consider that this corresponds to the methods section
Response: We will revise it in the manuscript
- Line 253: I notice that in the results section, you use past and present tenses. I suggest using the present tense.
Response: Thank you for highlighting. We will adjust this in revised manuscript.
- Lines 267-269: You state that Q and NEP are more sensitive to changes in precipitation than ET and GPP. You should also consider how climatic conditions before wet or dry years affect the responses of water and carbon fluxes, as well as their responses after dry or wet years, to examine potential lag effects. In this context, it is not clear how groundwater buffers drought impacts based on the results presented in Fig. 8 (Lines 373–375).
Response: In WaSSI, water storage is simulated through soil moisture dynamics. When examining years with low precipitation, we observed that soil water carried over from previous wetter years can partially buffer hydrological responses, which may explain the reduced sensitivity in some watersheds. Q was sensitive to Precip because ET is relatively stable.
However, a detailed analysis of lag effects—such as how wet or dry conditions influence subsequent water and carbon fluxes—would require additional diagnostics and is beyond the scope of the current study.
- Figure 6: Precipitation is not typically considered an ecosystem flux
Response: Thank you for highlighting. We will adjust this in revised manuscript.
- Figures 8 and 9: I suggest presenting the anomalies as percentages or standardized anomalies to better account for spatial variability across Germany.
Response: Thank you for the suggestion. Presenting anomalies as percentages or standardized values would indeed help account for spatial variability. However, implementing this transformation for all watersheds would require additional data processing beyond the resources available for the current revision. We appreciate the recommendation and will consider incorporating standardized anomaly analyses in future work.
- Line 288: What are the implications of crop irrigation on water yield and carbon sequestration response to dry/wet years?
Response: The current WaSSI setup does not include crop irrigation, so irrigation effects are not represented in our simulations. However, irrigated lands may have higher LAI which was used in WaSSI model for characterizing land surface conditions and ET rates. In general, we expect that irrigation would increase local water yield due to deep groundwater withdrawal and higher carbon sequestration because of higher ET and productivity.
- Lines 411-413: I think this sentence does not correspond to the conclusions section.
Response: Thank you for highlighting this we will move it to the discussion section in the revised manuscript.
Technical corrections:
- Line 52: Add space.
Response: We will revise it in the manuscript
- Line 108: I guess the correct reference is “Fan et al. (2016)”
Response: We will double check and revise it in the manuscript
- Line 139: Add a space in “of 2018” and “100 m”. This typo is found throughout the document.
Response: We will revise it in the manuscript
- Please check whether the figure colors are suitable for color-blind readers.
Response: We will double check
Citation: https://doi.org/10.5194/egusphere-2025-1629-AC2
-
AC2: 'Reply on RC1', Karim Pyarali, 30 Nov 2025
-
RC2: 'Comment on egusphere-2025-1629', Anonymous Referee #2, 01 Oct 2025
In this manuscript, the authors validate the WaSSI (Water Supply Stress Index) model for the case of Germany. Since this model has typically been applied to other study areas (i.e., the conterminous United States, Mexico, Rwanda, and Burundi), this application represents an innovative contribution. The study is also valuable in clarifying some of the dynamics behind the spatial and temporal variations of the ecosystem services considered in the study area. Nevertheless, a number of gaps are present, and taken together, they make it difficult to fully understand the methodologies and the results described in this work. In particular, some points and logical steps would benefit from a more detailed explanation in order to strengthen the overall clarity and robustness of the study. My review mainly focuses on these aspects.
In conclusion, I consider the manuscript suitable for publication, provided that the general revision suggested are carefully addressed.
General comments
- While reading the manuscript, I had the impression that the term “flood” is sometimes used to refer to a “high precipitation event” (e.g., line 372) or an “extremely wet year” (e.g., line 297). However, the term “flood” typically refers to the inundation resulting from an excess of water that causes normally dry areas to be submerged. It does not simply indicate heavy rainfall events or periods of above-average precipitation. I would therefore suggest reviewing the manuscript to ensure that the term “flood” is used correctly and, where necessary, replacing it with more precise terms or expressions.
- I think it would be important to consistently include references to the datasets used in the text. I would therefore suggest checking this aspect throughout the manuscript—for example, at line 164 (FLUXNET2015) and line 177 (MOD17A2HGF).
- Referring to Figure 4c, I found it a bit difficult to understand how, in some areas, actual evapotranspiration could exceed potential evapotranspiration. For readers who are not experts on the topic, the intuitive expectation would be that actual evapotranspiration is less than or equal to potential evapotranspiration. It might be worthwhile to explain and comment on this difference between the two variables, as this could help readers better follow the results.
- I believe that certain essential details are missing in the description of the procedures, particularly in some steps that are crucial for understanding the methodology. Specifically, the following aspects would benefit from further elaboration:
- Lines 145-146: a more detailed explanation of what the quality checks consisted of could improve the clarity of both the procedure and the results.
- Lines 158-160: for transparency and clarity, it could be helpful to provide further details about why those specific stations were selected, why not more were included, and how the choice of different stations might affect the results.
- Lines 164-165: a short explanation of how corrections and gap filling were carried out could be useful.
- Results and Discussion Section lack some important steps and information. These missing elements are essential to fully grasp the reasoning that supports the results and to properly assess their applicability in different contexts:
- In the Discussion section, I did not find any direct reference to Figure 6. It might be useful to elaborate on and comment on this figure, since it is the only one showing the temporal evolution of the variables considered.
- I think that from the presentation of the results, it is not clear how “buffers developed from the previous year can play a significant role in mitigating this effect”, particularly when discussing the sensitivity of ecosystem services to extreme events (lines 318–319). I believe it would be important to elaborate on this point in the Results section and, if possible, refer to the corresponding figures in the Discussion chapter.
- Line 320: it may be useful to further clarify why the model can be applied to the whole Central Europe. As it is currently written, it is not entirely clear how the procedures and conclusions could also be applied to areas beyond the specific study region (i.e., Germany).
Specific comments
- I am not very familiar with the WaSSI model, and I found it challenging to fully understand what it is and how it works. While some information is provided, it appears scattered across different parts of the manuscript. I think that an initial, more comprehensive presentation of the model—beyond what is already included—would be very helpful to better frame the analyses and to facilitate the interpretation of the results. This could include its main aim, the study areas considered, the way it operates, and other relevant details.
- In the abstract, a lot of results are described and explained. I think it might be helpful to more clearly highlight the main novelties and contributions introduced by this work.
- Please consider adding a section describing the study area (climate, land use, etc.)
- Line 15: you may consider briefly clarifying what is meant by “ecosystem services” for readers less familiar with the concept.
- It would improve readability if acronyms were defined when they first appear in the text. For example, “MODIS” and “CGLS” (lines 125 and 127) are introduced without prior definition.
- Line 141: providing a short explanation of why exactly 10 classes were chosen, and whether you considered different numbers, might help clarify the procedure.
- Line 145: including the number of removed pixels could be an informative detail.
- Lines 165-169: this section might be difficult to follow for readers less familiar with the topic. Expanding the explanation with more details could make it clearer.
- In Section 3.1, I think it would be very helpful to include a comparison between the performance metrics obtained for the different variables (discharge, ET, GPP) in this study and those reported in the literature from other studies applying the same or similar models (if available). Providing this context could help to better clarify the results and support the applicability of the WaSSI model to new study areas.
- Figure 2: adding a legend to indicate the meaning of the two colours could improve the clarity of the plots.
- Figure 4: you may consider including in the figure the names of the regions mentioned in the text, or finding a way to highlight them. This would make the reading and the analysis of the figure much easier.
- Lines 316-319: referring explicitly to the relevant tables/figures in the text could make the discussion clearer.
- Lines 324-327 and 333-336: a more detailed explanation of the influence of the different factors could add clarity.
- Line 339: explaining why results are weaker for the Lackenberg Forest station, or what the reasons can be, could improve transparency.
- Line 340 and 341: the meaning of the terms “complex” and “complicated” in this context is not entirely clear; considering alternative synonyms or more specific wording may help.
Technical comments
- I warmly suggest to check that the figures are accessible also for readers with colour-vision deficiencies. Alternative colour scales might improve clarity.
- Figure S1: you might consider modifying the colour scale (as noted above) and/or using different marker shapes for each category to increase readability.
- Please double-check punctuation when separating sentences across the manuscript. In some cases, a full stop is missing (e.g., line 36, between “interconnected reasons” and “two of them”), while in others a full stop is used where a comma or similar punctuation might be more appropriate (e.g., line 53, before the sentence starting with “Which negatively affects”). In my opinion, this would strongly improve the readability of the manuscript.
Citation: https://doi.org/10.5194/egusphere-2025-1629-RC2 -
AC1: 'Reply on RC2', Karim Pyarali, 08 Nov 2025
Thank you for taking the time to share your feedback. We truly appreciate your valuable insights and will use them to guide our improvements. We have provided responses to each of your comments (highlighted in bold and italics). At this stage, the comments have not been incorporated into the manuscript, as per the editor’s instructions to refrain from making revisions at this time.
General comments
- While reading the manuscript, I had the impression that the term “flood” is sometimes used to refer to a “high precipitation event” (e.g., line 372) or an “extremely wet year” (e.g., line 297). However, the term “flood” typically refers to the inundation resulting from an excess of water that causes normally dry areas to be submerged. It does not simply indicate heavy rainfall events or periods of above-average precipitation. I would therefore suggest reviewing the manuscript to ensure that the term “flood” is used correctly and, where necessary, replacing it with more precise terms or expressions.
Response: Thank you for highlighting this. We will change the term “flood” accordingly in the revised manuscript.
- I think it would be important to consistently include references to the datasets used in the text. I would therefore suggest checking this aspect throughout the manuscript—for example, at line 164 (FLUXNET2015) and line 177 (MOD17A2HGF).
Response: Thank you for highlighting this. We will include this change in the revised manuscript.
- Referring to Figure 4c, I found it a bit difficult to understand how, in some areas, actual evapotranspiration could exceed potential evapotranspiration. For readers who are not experts on the topic, the intuitive expectation would be that actual evapotranspiration is less than or equal to potential evapotranspiration. It might be worthwhile to explain and comment on this difference between the two variables, as this could help readers better follow the results.
Response: We agree with this comment and will further clarify this in the revised manuscript.
- I believe that certain essential details are missing in the description of the procedures, particularly in some steps that are crucial for understanding the methodology. Specifically, the following aspects would benefit from further elaboration:
- Lines 145-146: a more detailed explanation of what the quality checks consisted of could improve the clarity of both the procedure and the results.
Response: The LAI data is provided by Copernicus, which applies a very detailed and complex Quality Check on the dataset. We can further elaborate on this process and share the source as in-text citation for readers.
- Lines 158-160: for transparency and clarity, it could be helpful to provide further details about why those specific stations were selected, why not more were included, and how the choice of different stations might affect the results. \
Response: We appreciate the opportunity to clarify our station selection criteria. In addition to minimising anthropogenic influences, the chosen upstream stations were selected to ensure spatial coverage across Germany, representing the country’s major climatic zones, land use, and land cover types. We also prioritised stations with long and continuous discharge records. We will add this explanation to the manuscript. We believe this additional information will help readers better understand the rationale behind the station selection and the robustness of our validation results.
Lines 164-165: a short explanation of how corrections and gap filling were carried out could be useful.
Response: Thank you for the helpful suggestion. The gap filling and corrections in FLUXNET2015 are conducted using standardised procedures described in Pastorello et al. (2020). We will add a brief note to the manuscript to clarify this point explicitly.
- Results and Discussion Section lack some important steps and information. These missing elements are essential to fully grasp the reasoning that supports the results and to properly assess their applicability in different contexts:
- In the Discussion section, I did not find any direct reference to Figure 6. It might be useful to elaborate on and comment on this figure, since it is the only one showing the temporal evolution of the variables considered.
Response: There is a detailed explanation on temporal evolution of the variable from line 264 – 273 with a direct reference to Figure 6 on line 273.
- I think that from the presentation of the results, it is not clear how “buffers developed from the previous year can play a significant role in mitigating this effect”, particularly when discussing the sensitivity of ecosystem services to extreme events (lines 318–319). I believe it would be important to elaborate on this point in the Results section and, if possible, refer to the corresponding figures in the Discussion chapter.
Response: Thank you for highlighting this, we will further elaborate on it in the revised manuscript.
- Line 320: it may be useful to further clarify why the model can be applied to the whole Central Europe. As it is currently written, it is not entirely clear how the procedures and conclusions could also be applied to areas beyond the specific study region (i.e., Germany).
Response: We find this comment very interesting and will add further clarification in the revised manuscript.
Specific comments
- I am not very familiar with the WaSSI model, and I found it challenging to fully understand what it is and how it works. While some information is provided, it appears scattered across different parts of the manuscript. I think that an initial, more comprehensive presentation of the model—beyond what is already included—would be very helpful to better frame the analyses and to facilitate the interpretation of the results. This could include its main aim, the study areas considered, the way it operates, and other relevant details.
Response: Thank you for sharing this perspective. We will elaborate further on WaSSI model in the revised manuscript using your suggestions.
- In the abstract, a lot of results are described and explained. I think it might be helpful to more clearly highlight the main novelties and contributions introduced by this work.
Response: The results shared in the abstract respond to the research questions we have for this study. They highlight the quantification of stocks and flow of ecosystem services in Germany. Nevertheless, we will further emphasize on the main novelty of this study, which is that a relatively simple modelling approach is adequate to analyse carbon and water response to climatic variability.
- Please consider adding a section describing the study area (climate, land use, etc.)
Response: Sure, we will add this section in the revised manuscript.
- Line 15: you may consider briefly clarifying what is meant by “ecosystem services” for readers less familiar with the concept.
Response: Sure, we will add some examples of ecosystem services in the revised manuscript.
- It would improve readability if acronyms were defined when they first appear in the text. For example, “MODIS” and “CGLS” (lines 125 and 127) are introduced without prior definition.
Response: We agree with you, thank you for flagging the acronyms we missed to define.
- Line 141: providing a short explanation of why exactly 10 classes were chosen, and whether you considered different numbers, might help clarify the procedure.
Response: Sure, this is valuable comment. The selection of 10 classes was based on the availability of water-use efficiency (WUE) parameters and their correspondence to the major biomes represented in the dataset. These 10 classes encompass all dominant ecosystem types across the study. We will add this explanation in the revised manuscript.
- Line 145: including the number of removed pixels could be an informative detail.
Response: Thank you for this thoughtful suggestion. Unfortunately, estimating this information would require additional data processing and computational resources beyond the scope of this study. However, all quality-control and masking procedures were applied following the provided guidelines and best-practices.
- Lines 165-169: this section might be difficult to follow for readers less familiar with the topic. Expanding the explanation with more details could make it clearer.
Response: Thank you for highlighting this, we will adjust it in the revised manuscript and briefly add more details. However, the eddy flux dataset is indeed a complex topic and a detailed description would be out of scope for this study.
- In Section 3.1, I think it would be very helpful to include a comparison between the performance metrics obtained for the different variables (discharge, ET, GPP) in this study and those reported in the literature from other studies applying the same or similar models (if available). Providing this context could help to better clarify the results and support the applicability of the WaSSI model to new study areas.
Response: Thank you for this suggestion. We agree that comparing our model performance with results from other studies could provide useful context. However, similar large-scale applications of model for estimation of discharge, ET, and GPP over the entire Elbe basin are very limited, directly comparable studies are difficult to find. Please feel free to share any studies that you feel would be meaningful. Additionally, we aim to keep Section 3.1 focused on presenting the results of this study, while broader contextual comparisons are more suitable for the Discussion section. We will therefore consider including a brief comparative discussion there to highlight the relative performance of our results within the context of available literature.
- Figure 2: adding a legend to indicate the meaning of the two colours could improve the clarity of the plots.
Response: Thank you for the suggestion. A legend indicating the meaning of the two colours is already included in the first subplot (Station ID: Bentfeld) and applies to all stations shown in Figure 2.
- Figure 4: you may consider including in the figure the names of the regions mentioned in the text, or finding a way to highlight them. This would make the reading and the analysis of the figure much easier.
Response: Sure. We will take care of it in the revised manuscript.
- Lines 316-319: referring explicitly to the relevant tables/figures in the text could make the discussion clearer.
Response: Thank you for the suggestion. We will take care of it in the revised manuscript.
- Lines 324-327 and 333-336: a more detailed explanation of the influence of the different factors could add clarity.
Response: We appreciate the reviewer’s interest in a more detailed explanation. We will add further details where possible to better explain the underlying processes in the revised manuscript
- Line 339: explaining why results are weaker for the Lackenberg Forest station, or what the reasons can be, could improve transparency.
Response: Thank you for the suggestion. We will take care of it in the revised manuscript.
- Line 340 and 341: the meaning of the terms “complex” and “complicated” in this context is not entirely clear; considering alternative synonyms or more specific wording may help.
Response: Thank you for highlighting this, we will adjust it in the revised manuscript.
Technical comments
- I warmly suggest to check that the figures are accessible also for readers with colour-vision deficiencies. Alternative colour scales might improve clarity.
Response: Thank you for highlighting these points. We will take care of it in the revised manuscript.
- Figure S1: you might consider modifying the colour scale (as noted above) and/or using different marker shapes for each category to increase readability.
Response: Thank you for highlighting these points. We will take care of it in the revised manuscript.
- Please double-check punctuation when separating sentences across the manuscript. In some cases, a full stop is missing (e.g., line 36, between “interconnected reasons” and “two of them”), while in others a full stop is used where a comma or similar punctuation might be more appropriate (e.g., line 53, before the sentence starting with “Which negatively affects”). In my opinion, this would strongly improve the readability of the manuscript.
Response: Thank you for highlighting these points. We will take care of it in the revised manuscript.
Citation: https://doi.org/10.5194/egusphere-2025-1629-AC1
Viewed
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 1,313 | 76 | 33 | 1,422 | 36 | 37 | 39 |
- HTML: 1,313
- PDF: 76
- XML: 33
- Total: 1,422
- Supplement: 36
- BibTeX: 37
- EndNote: 39
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
Pyarali et al. simulate how different land cover types and climate variability – wet and dry years – modulate multiple ecosystem processes and services using the Water Supply Stress Index (WaSSI) model in Germany. The study contributes to understanding the spatio-temporal variability of the provision of key ecosystem services such as water yield and carbon sequestration, as well as their anomalies during extreme wet and dry years, at a national scale, using an ecosystem model that simulates the coupling between water and carbon cycles. Additionally, the manuscript can provide new insights into the potential loss of ecosystem services provision under future climate projections in Germany.
While the manuscript is well written and organized, I see some issues that, in my view, need to be addressed before it can be considered for publication in HESS. Specifically: (i) I found it difficult to follow the description of the model evaluation given the limited level of detail provided on validation; (ii) the manuscript would be strengthened by a more explicit discussion of how the areal extent of each land cover type influences the provision of ecosystem services; (iii) the characterization of extreme wet and dry years is based only on precipitation anomalies, which I find too narrow.
Major comments:
Minor comments:
Technical corrections: