the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Seasonal Cycle Biases in DGVM Simulations of Double-Cropping Systems: A Case Study in the Huang-Huai-Hai Plain
Abstract. Global dynamic vegetation models (DGVMs) are essential tools for studying the changes in terrestrial ecosystems and their responses to climate change and human activities. However, these models exhibit substantial uncertainties when applied to croplands, particularly in regions with multiple cropping systems. These uncertainties arise from variations in planting types and phenology, which are influenced by sowing and harvesting schedules. This study focused on the phenological estimation errors of DGVMs in typical double - cropping agricultural regions. The Huang - Huai - Hai Plain in eastern China was chosen, which is one of the most important grain-producing areas with mainly winter wheat-summer crop rotation. A comparative analysis was conducted between the seven models from the TRENDY project and three remote sensing observations over last two decades. The results indicate that remote sensing vegetation indices consistently exhibit a typical bimodal structure in the study area, with peaks in April and August, corresponding to the growth peaks of the two-season crops. However, none of the DGVMs successfully capture this bimodal pattern. Given that multiple cropping systems are widespread in middle- and low-latitude regions with favorable water and temperature conditions, improving the simulation capabilities of DGVMs in such areas is an urgent and critical issue for advancing global vegetation modeling.
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Status: final response (author comments only)
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RC1: 'Comment on egusphere-2025-4997', Anonymous Referee #1, 09 Feb 2026
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AC1: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Response of review “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”
Dear Reviewer,
Thank you very much for your time and insightful suggestions. Your in-depth discussion has been especially valuable for improving this paper. We have also provided detailed responses to address your concerns. Although some of the results might be expected from a theoretical perspective, the goal of this paper is to quantify current deficiencies and thereby draw attention to the need for improving the representation of multi-cropping regions in DGVM development. This is of great importance for the advancement of Earth system models. Below are our point-by-point responses to your comments.
Thanks again.
Tiexi CHEN and co-authors
General remarks
The manuscript compares simulation results from the TRENDY model ensemble against remote sensing products for the Huang-Huai-Hai Plain, focusing on double-cropping systems. While the paper is well written, I am sorry to say that I have fundamental concerns about the scientific contribution that lead me to recommend rejection.
My primary concern is that the paper's central finding (TRENDY models fail to reproduce bimodal LAI patterns characteristic of double-cropping) provides limited scientific insight. These models do not implement double-cropping mechanisms. Comparing model results against data for phenomena they do not simulate is neither surprising (expected outcome confirmed) nor novel. Waha et al., (2025), whom the authors cite, already established this limitation globally. Since the model structures are not discussed it is also not of diagnostic relevance (nothing is learned on how to improve the models specifically).
In my opinion, the comparison therefore lacks the scientific value necessary for publication.
I have considered whether a comparison of the LAI patterns from the different remote sensing products might have standalone value independent of the model comparison. However, the manuscript does not establish that this regional documentation is novel, which would need to be verified. Furthermore, this would in my opinion need the connection of the patterns to broader implications appropriate for Biogeosciences (e.g., biogeochemical cycles or Earth system science). Additionally, several methodological issues (detailed below) would need to be resolved.
The manuscript also presents analyses of greening trends (Sections 3.1-3.2, Figures 3-7) that could potentially provide scientific insight, as models should capture vegetation responses to climate and management changes. However, this analysis suffers from similar issues: The models are grouped based on how their results compare against the remote sensing data but structural differences that might explain divergent behaviors are not explored, and the analysis remains descriptive rather than diagnostic.
I do not believe major revisions can address these issues. The paper would need to be reconceived as either: (a) a diagnostic analysis of models that attempt to simulate double-cropping (requiring different models than the TRENDY ensemble), (b) if it is not too similar too existing works, a purely observational documentation of remote sensing products (requiring different focus), or (c) a diagnostic analysis of what distinguishes models showing greening versus browning trends (requiring systematic structural comparison). A combination of b and c would also be possible. However, all of these would constitute a substantially different study rather than a revision.
I hope that the specific comments below, which detail the technical and methodological issues, help the authors in reconsidering how to present this work.
Response
We greatly appreciate the reviewer’s thorough and insightful evaluation of our manuscript, particularly the systematic and in-depth comments on the core rationale and scientific contribution of this work, rather than focusing solely on technical details. Our research team is an experienced user of Dynamic Global Vegetation Models (DGVMs), with a long-term focus on eco-climatic process modelling, including the estimation of vegetation productivity and attribution analysis of vegetation greening. In recent years, we have paid special attention to the modelling and optimization of agricultural land management processes. The core objective of this manuscript is to identify the specific biases introduced into DGVM simulations by the lack of explicit representation mechanisms for double-cropping processes.
As the reviewer correctly points out, the finding of this study is an "expected" result, which may lead to an insufficient scientific contribution. However, a critical question we seek to address is: why has there been no significant progress in resolving this model limitation to date? We argue that one core reason is the lack of a broad consensus in the research community on the severity of this issue, which necessitates a systematic case study in a representative region to concretize the impacts of this limitation. Since remote sensing information can extract the planting intensity of crops, and the potential for multiple cropping based on accumulated temperature, along with real-world constraints, can theoretically be used to assess cropping systems, we have noticed that some models have already considered multiple crop types. For example, the LPJ-guess model classifies over a dozen crop types. This means that the differences between crop types are gradually gaining attention. However, for multiple cropping, no systematic improvements have been made so far. Moreover, we believe that improvements in planting intensity may be at least equally important as crop classification.
The simulation accuracy of DGVMs is fundamental to multiple core research directions in terrestrial ecosystem modelling, which are detailed in the following three aspects:
- Attribution of vegetation change: Represented by the classic studies of Piao et al. (2015) and Zhu et al. (2016), the core methodological framework in this field relies on multi-scenario simulations using DGVMs, and quantifies the contribution of different driving factors via the differential analysis of scenario outputs. This is also one of the landmark achievements of the TRENDY project.
- Uncertainty sources of vegetation greening: As stated in Chapter 3 of the IPCC AR6 Working Group I Report (Masson-Delmotte et al., 2021), land management is a key source of low confidence in the global attribution of vegetation greening, as it has become the dominant driver over CO₂ fertilization in some regions. [Original quote: "The main driver of the observed increase in the amplitude of the seasonal cycle of atmospheric CO₂ is enhanced fertilization of plant growth by the increasing concentration of atmospheric CO₂ (medium confidence). However, there is only low confidence that this CO₂ fertilization has also been the main driver of observed greening because land management is the dominating factor in some regions. Earth system models simulate globally averaged land carbon sinks within the range of observation-based estimates (high confidence), but global-scale agreement masks large regional disagreements. {3.6.1}"]
- Requirements for coupled Earth System Model (ESM) simulations: The IPCC Seventh Assessment Report (AR7) is currently in the drafting phase, and the simulation accuracy of ESMs is highly dependent on the robust representation of terrestrial vegetation systems by DGVMs to establish reliable land-atmosphere coupling relationships. The lack of double-cropping process representation is a critical flaw in current DGVM cropland simulations. Double-cropping occupies 17.42 % (2.62×106 km2) of global croplands which could not be ignored (Zhang et al., 2021).
This issue is particularly pronounced in regions with extensive multiple-cropping systems, most notably during the summer harvest-sowing transition period. Models fail to capture the rapid shift from peak vegetation cover to bare soil/seedling states, which introduces large biases into simulations of land surface biogeochemical cycles and energy balance. Furthermore, as global warming expands the climatically suitable areas for multiple cropping toward higher latitudes, accurate representation of multiple-cropping processes has become an urgent unresolved issue in climate change impact research.
It should be noted that not all DGVMs are open-source. We are currently working on the improvement of two models: the open-source Community Land Model version 5.0 (CLM5.0), and the VEGAS model accessed via academic collaboration (with related findings published in Zhou et al., 2022, same first author).
In this revised manuscript, we will further refine the presentation of the patterns used in this paper in accordance with the reviewers' suggestions.
As the reviewer notes, the three recommendations (a)-(c) have clarified our core future research directions, and our team is already advancing work on several of these aspects. The core positioning of this study is as a foundational preliminary work for this research direction, with the central goal of systematically revealing the key limitations of current models – this is the core scientific value of our work. We sincerely hope that this research positioning can be recognized by the reviewer and the journal editors. Meanwhile, based on the reviewer’s suggestions on the scientific contribution of this work, especially Major Comments 2 and 3, we have provided more systematic and in-depth elaboration in the revised manuscript to comprehensively enhance the scientific contribution of this study.
Major comments
1、Missing assessment of model capabilities. The manuscript lacks an overview of TRENDY model structures and the modelling protocol. It is my understanding that such an overview would immediately reveal that the majority of TRENDY models—with the exception of LPJmL and certain versions of ORCHIDEE—cannot simulate double-cropping systems. Furthermore, even these two models do not appear to activate double-cropping functionality under the TRENDY protocol.
This is a fundamental issue for the paper's framing: the authors compare model outputs to observations of a phenomenon the models do not simulate, then interpret the mismatch as model failure. The finding that TRENDY models fail to reproduce the bimodal LAI pattern (L176-184) is therefore neither surprising nor informative and only confirms what a review of model documentation would reveal. The authors cite Waha et al. (2025), who specifically highlight that multiple cropping "is hardly accounted for" in global land use models.
However, this is not picked up when interpreting their results. This creates a misleading impression that models attempted but failed to capture double-cropping, rather than acknowledging they were not designed to do so.
A table summarizing each model's cropland representation (single/multiple crops per year, crop types simulated, phenology scheme) would make this limitation explicit. However, it would also show that the comparison is of limited diagnostic value. If a mechanism is entirely absent from a model, the amount that can be learned about parameterisation and model processes is limited. This represents a fundamental conceptual issue rather than a missing detail.
Additionally, the introduction (lines 63-66) mentions that "cropping intensity is generally expressed on a scale of 1-3" but it is not clear to me whether this refers to observational datasets, model inputs, or model capabilities. This ambiguity extends throughout the manuscript. As far as I can tell, the authors never explicitly state that TRENDY models do not simulate double cropping for this region, leaving readers to infer this important limitation. The authors should also clarify what cropping intensity the HYDE land-use forcing (used by TRENDY) assigns to the Huang-Huai-Hai Plain and how this is handled by TRENDY.
Response
We sincerely apologize for the ambiguity in the original manuscript that caused misunderstanding for the reviewer. The core intent of this study is not to argue that "models attempted to simulate double-cropping but performed poorly", but to reveal the specific simulation biases arising from the lack of explicit representation of double-cropping processes in current DGVMs, and further explore how models can effectively represent multiple-cropping systems (cropping intensity 2-3). This core positioning was stated in the original discussion section with the sentence: "This discrepancy arises because current DGVMs lack explicit mechanisms for double-cropping systems."
In the revised manuscript, we highlight and explicitly clarify this core research positioning in accordance with the reviewer’s comments. For model selection, the TRENDY multi-model ensemble is the most widely used framework in global vegetation dynamic modelling, with the most complete publicly available datasets, and was therefore selected as the core analysis object for this study.
In the revised manuscript, we have explicitly stated this positioning at the outset of the objective subsection in the Introduction, and clarified that cropping intensity information in related studies is extracted from remote sensing phenological cycles. The revised text is as follows:
“Intensifying multiple cropping is considered an important means of increasing food production without expanding cropland area (Wu et al., 2018). As global warming expands the climatic potential for multiple cropping toward higher latitudes, understanding and modeling these systems becomes increasingly urgent. However, processes related to multiple cropping are rarely represented in current DGVMs. Cropping intensity is generally expressed on a scale of 1-3, corresponding to single, double, and triple cropping, respectively, and can be determined by extracting phenological cycles from remote sensing data. Yet, because multiple cropping systems are often complex and interspersed with intermittent fallow periods, many such areas are not stably cultivated over long timescales (Liu, 2021). Consequently, most DGVMs still simulate croplands under a single-cropping assumption, leaving a critical gap in our ability to assess the biogeophysical and biogeochemical impacts of agricultural intensification. To address this, we selected the Huang-Huai-Hai Plain, a highly representative double-cropping region, as our study area. Since the 1980s, this region has been dominated by a winter wheat–summer crop double-cropping system. The objective of this study is to quantify the biases introduced by the single-cropping assumption in current DGVMs when simulating vegetation seasonality under intensive double-cropping management, thereby highlighting the urgent need to better represent agricultural practices in land surface models.”
In addition, we added the following model information in table 2 as:
Table 2. Spatial Resolution, Temporal Resolution and Temporal Coverage of chosen Leaf Area Index datasets. The abbreviations represent the dataset names that appear later in the text.
Dataset Name
Spatial Resolution
Temporal Resolution
Temporal Coverage
Abbreviation
cropland included
Single/multiple cropping
GIMMS-LAI4g
1/12°
half monthly
1982-2020
LAI4g
MOD15A2H
500m
8 day
2000.feb-2023
MOD15
GLASS-LAI
0.05°
8 day
2000.feb -2022
GLASS
ED
0.5°
monthly
1700-2023
ED
NAN
NAN
ISAM
0.5°
monthly
1700-2023
ISAM
YES
Single
LPJ-GUESS
0.5°
monthly
1700-2023
LPJ-GUESS
YES
Single
LPJml
0.5°
monthly
1700-2023
LPJml
YES
Single
LPXbern
0.5°
monthly
1700-2023
LPXbern
YES
Single
ORCHIDEE
0.5°
monthly
1700-2023
ORCHIDEE
YES
Single
VISIT
0.5°
monthly
1860-2023
VISIT
YES
Single
Meanwhile, we have compiled the structural characteristics of cropland simulation for each model in the revised manuscript, and added Table to summarize the representation capacity of each model for cropland ecosystems. Additionally, regarding the current issue of Multi-Season-Cropping farmland, we conducted further literature research and presented our findings in the Discussion section.
We investigated each model, including both the model development papers and the papers citing the models, as detailed in the list. Unfortunately, we are currently unable to fully clarify how each model handles cropland information in detail. We can only determine whether they attempt to include multiple cropping. Based on current understanding, whether multiple cropping is included is the main reason for the limited simulation capability in this region, rather than whether crop types are refined.
Table 3. Overview of the simulation capabilities for Cropland of the selected models from Trendy v12
Dataset Name
Cropland module
Crop Functional Type
Phenology
Irrigation module
Fertilization Module
ED
NAN
ISAM
YES
Maize (C4)、Wheat、Rice、Soybean(C3)
Defined by accumulated temperature
YES
YES
LPJ-GUESS
YES
Separate crop phenology schemes on a daily time-step are present for simulations with and without N-limitation. Cropland without N-limitation is represented by eleven crop PFTs (temperate cereals, rapeseed, pulses, sugarbeet, maize, soybean, tropical cereals, sunflower, peanut, cassava and rice), simulated separately (without inter-PFT competition) and two grass PFTs (competing C3 and C4 grass) as cover crop between harvest and sowing. The same grass PFTs are used to represent pastures. Currently, two crop PFTs are defined for N-limited simulations (wheat and maize).
Defined by accumulated temperature and precipitation
YES
YES
LPJml
YES
In LPJmL4, 12 different annual CFTs are simulated (Table S10), similar to Bondeau et al. (2007)
with the addition of sugar cane. The basic idea of CFTs
is that these are parameterized as one specific representative crop (e.g. wheat, Triticum aestivum L.) to represent a broader group of similar crops (e.g. temperate cereals)
The phenological development of crops in LPJmL4 is driven by temperature through the accumulation of growing degree days and can be modified by vernalization requirements and sensitivity to daylength (photoperiod) for some CFTs and some varieties.
YES
YES
LPXbern
YES
The farmland and the pasture share the common herbaceous PFT, without distinguishing specific crop types such as wheat, corn, or rice, and there is no dedicated crop PFT.
The core physiological process framework is consistent with the natural herbal PFT.
NAN
YES
ORCHIDEE
YES
Define two specific agricultural PFTs: Agricultural C3 grass and Agricultural C4 grass
ORCHIDEE assumes
that all C3 agriculture is a perennial prairie and does not
account for harvest.
NAN
NAN
VISIT
YES
The global farmland is divided into three core functional types:
1.C3 crop type, represented by crops such as wheat, which adopts the parameterization scheme of C3 plant photosynthetic physiology;
2. C4 crop type, represented by crops such as corn in tropical/subtropical regions, which is adapted to the photosynthetic and water utilization characteristics of C4 plants;
3.Rice field type specifically designed for the rice-growing areas in the Asian monsoon region. In addition to the basic crop physiological simulation, it additionally couples the seasonal flooding hydrological process and the exclusive module for rice field CH₄ emissions.
In response to the agricultural production characteristics of different climate zones, differential planting systems and phenological-driven schemes are adopted. The core rules are as follows:
1. In temperate regions: A one-year cropping system is implemented, with the growth cycle driven by temperature thresholds:
◦ The core indicators for initiating and ending the growing season are the monthly average temperature of 5°C as the critical value;
◦ When the growth season begins, a fixed amount of carbon is added to the crop biomass reservoir to simulate the initialization process of sowing/transplanting;
◦ When the surface temperature is below the critical value of 5°C, the crop harvest process is triggered.
2. In tropical regions (average annual temperature > 20°C): A continuous annual cropping system is adopted, without setting seasonal start and end periods for growth. Sowing and harvest occur continuously at a constant rate each month.
NAN
NAN
2、Overgeneralization of model characteristics. The authors do not acknowledge the structural differences in cropland representation between the TRENDY models. For example, Figures 5- 6 present all model outputs together without differentiating by model structure. These structural differences likely explain some of the inter-model spread in Figures 5-6 but remain unexplored. Models differ in fundamental ways that could influence LAI seasonal patterns:
Phenology schemes: Some models use grass-like phenology for crops (baseline ORCHIDEE) while others implement crop-specific phenology with heat unit accumulation and photoperiod responses (ORCHIDEE-CROP, LPJmL).
1)Crop functional type representation: Models range from generic C3/C4 categories to multiple crop-specific functional types with distinct parameterizations.
2)Management representation: Some models lack explicit management routines—crops follow natural phenology without prescribed sowing dates, fertilization schedules, or harvest triggers (baseline ORCHIDEE)—while others include these processes (ORCHIDEE-CROP, LPJmL).
3)Land use models—including TRENDY models—"primarily assume monocropping" (Waha et al., 2025), meaning they simulate only a single crop per grid cell per year. While some models like LPJmL and LPJ-GUESS can represent multiple crop types within a grid cell, TRENDY simulations do not implement sequential cropping (two crops harvested from the same field within one year). This fundamental limitation means models should not reproduce the bimodal LAI pattern characteristic of winter wheat-summer maize double-cropping in the study region. If they would reproduce these patterns, they would be right for the wrong reasons.
In my opinion, the analysis needs to differentiate models depending on these structural characteristics and document their capability to simulate double cropping. Otherwise, the analysis cannot meaningfully interpret inter-model differences or explain why models collectively fail to capture the observed seasonal pattern.
Response
We thank the reviewer for this valuable comment. As you mentioned, these models have begun to focus on the vegetation changes brought about by phenology (such as LPJ-GUESS and LPJmL), achieving this through crop responses to the climatic response cycles. However, multiple cropping itself disrupts the natural cycles. Whether multiple cropping can be realized depends on whether the water and heat conditions throughout the year support it, i.e., the potential for multiple cropping estimation. Currently, the Trendy model primarily assumes single-season cropping. The issue we wish to highlight is the lack of clarity introduced by single-season cropping at the regional scale. This is particularly important because these models are currently used as key data support and tools for calculating global greening and its attribution. The significant gaps in multiple cropping regions imply considerable errors, yet these errors are seldom addressed.
We hope to clearly highlight this issue in the paper, namely that the problems arising from the requirement of single cropping are highly significant at the regional scale and should be given due attention in the design.
3、Insufficient analysis of divergent greening trends. The manuscript documents substantial disagreement among models regarding greening trends (Figures 3-4, L145-155), with some models showing strong greening (LPX-Bern, ED) while others show browning (ISAM, LPJmL). I believe this assessment could have real merit and provide substantial scientific insight. However, the analysis only reports that the ensemble collectively “fails” to reproduce these trends without trying to understand why models disagree. Yet this could increase understanding of which processes or parameterizations are most important for simulating agricultural vegetation dynamics under climate change. The paper mentions potential drivers (CO₂ fertilization, nitrogen deposition, climate change, land management; L39-41, 239-240) but does not systematically evaluate how these are represented in different models. It would be interesting to know if for example models that show browning lack CO₂ fertilization effects on crops. Or if crop-specific versus grass-like phenologies are associated with better trend representation. Additionally, the conclusion that "DGVMs underestimate the contribution of croplands to regional greening trends" (L 283) appears to mix models with opposite behaviours together. Similar to major comment 2, I think an analysis of the structural differences between models (see the table suggested in major comment 1) in relation to greening performance would be beneficial. I would suggest grouping models at least by their trend direction and investigating what distinguishes "greening" from "no- greening" models. Such an analysis might help identify which model features are critical for capturing observed agricultural responses to global change. However, it would require the systematic structural comparison outlined in major comment 1. In my opinion this is a different study focused on diagnosing model differences rather than documenting failure.
Response
First, we would like to thank you for your insightful observations and analysis. The global vegetation change trends and their attribution are very important issues, and DGVMs seem to be the only reliable methods capable of simultaneously identifying driving factors and quantifying attribution. The directional differences in trends (both positive and negative) are an unexpected outcome that we did not anticipate. However, since we are currently only able to conduct validation analysis on the published data, the model structure can only be obtained from surveys. Therefore, we are uncertain how to approach a deeper exploration of the mechanisms behind these trends, and can only present the issue as it stands. The statement in L283 was inaccurate, so we have made adjustments and specifically addressed this in the discussion, hoping to draw attention to it. We are unsure whether similar response issues exist in other regions.
In the revision, we have removed the sentence: "DGVMs underestimate the contribution of croplands to regional greening trends." At the same time, the following content was added in the discussion section:
"There are significant discrepancies in the simulated trends, even showing contradictory growth and decline trends, while remote sensing LAI shows a relatively consistent growth trend. We are currently unable to provide a clear conclusion on why such large discrepancies exist in the trends, and which specific factors contribute to this. The absence of multiple cropping is just one of the potential influences. Given that DGVMs are important tools for attributing and quantifying global greening, the current inconsistency issue should receive sufficient attention."
BTW, stepping out of the scope of this paper, this is an open topic. Model development is a very challenging task, and the development teams of these models have made significant contributions. However, at the same time, objective conditions limit our ability to easily access model codes or participate in the design of comparison project plans. As a data-user researcher, our current research on model performance is still primarily focused on data-related issues. We also hope to be more involved in model modifications, but as mentioned earlier, the work we can participate in is mainly through open-source models.
4、Insufficient description of data processing methods. While the manuscript provides detailed descriptions of the remote sensing products (Section 2.2, L 90-103), it does not explain the aggregation methods used to standardize these datasets. The products have very different native resolutions—MODIS at 500m/8-day, GLASS at 0.05°/8-day, and GIMMS at 1/12°/semi- monthly—yet all are aggregated to 0.5°/monthly for comparison. The authors state only that datasets were "standardized" (line 101) without specifying:
(1)Temporal aggregation: How were 8-day or semi-monthly values converted to monthly? (e.g., mean, maximum, integrated LAI-days?)
(2)Spatial aggregation: How were fine-resolution pixels aggregated to 0.5°? (e.g., area- weighted mean, simple average?)
(3)Cropland masking: Was aggregation performed before or after applying the cropland mask? This matters substantially when cropland covers only a fraction of 0.5° cells. I am concerned that these choices could significantly affect the bimodal pattern the authors analyse. For example, monthly means vs. monthly maxima could alter the prominence of growth peaks. This could make a substantial difference but without the description of their methods the reader cannot know. I would recommend adding a subsection describing aggregation procedures, and a justification of the authors’ choices.
Response
We thank the reviewer for the rigorous and detailed professional comments on the data processing methods. Full disclosure of the standardized aggregation methods for multi-source data is a core prerequisite for ensuring the reproducibility of research results and the reliability of conclusions. We acknowledge the omission of method description in the original version, and fully agree with the reviewer’s professional judgment that the choice of processing workflow can significantly affect the analysis of the bimodal LAI pattern. We have completed the supplementation and revision of this section in response to the comments, with details as follows:
We have added a dedicated subsection Spatiotemporal Aggregation and Standardization of Multi-source Remote Sensing Data under Section 2.2 Remote Sensing Products in the manuscript, which clarifies the operational details for the three core questions raised by the reviewer one by one to ensure full reproducibility of the method:
Temporal aggregation method: For the 8-day resolution data from MODIS and GLASS, we first performed linear interpolation to daily resolution, and then calculated the arithmetic mean of all valid daily observations within each calendar month to derive the monthly LAI value. For the semi-monthly resolution GIMMS data, the monthly LAI value was represented by the arithmetic mean of the first and second half-month observations in the same month.
This method can smooth the random noise of single-period data while fully retaining the characteristic bimodal seasonal dynamics of the double-cropping system, and avoids the over-amplification of transition period signals caused by the maximum value composite method.
Spatial aggregation method: For the high-resolution raw data of MODIS (500 m) and GLASS (0.05°), the area-weighted averaging method was used to aggregate the data to the target 0.5° grid, rather than simple arithmetic averaging. This method eliminates the bias caused by the pixel area proportion of different resolution data, and ensures that the value of the 0.5° grid fully represents the mean cropland LAI of the corresponding region, which is completely matched with the grid scale of the TRENDY model outputs.
Implementation sequence of cropland masking: We adopted the workflow of aggregation followed by cropland masking. Mixed pixels are an unavoidable issue in scale conversion. It is difficult to find 0.5° grids with pure cropland cover in both model results and real-world remote sensing images. We therefore performed grid screening based on the 0.5° aggregated land use/cover percentage data. A grid was classified as a cropland grid in a given year when its cropland coverage exceeded 50%. If the grid was consistently classified as cropland throughout the study period, we considered it to have stable land use with no conversion, and included it in the cropland mask.
Through this method, we aim to extract the seasonal characteristics of croplands while retaining sufficient sample representativeness and preserving cropland information to the greatest extent possible. This workflow is applicable to both the RESDC land cover dataset and the HYDE land use dataset. We have also included the masking results based on the HYDE dataset in the Discussion section as a sensitivity analysis to test whether the HYDE-based cropland mask alters the observed bimodal pattern in the remote sensing data.
The Figure 1-3 is provided in the Supplementary Materials.
The differences in the Cropland masks produced by the two datasets are very small, and they do not have a significant impact on the bimodal structure of LAI in the farmland. We believe that the mask is not the cause of the seasonal differences in remote sensing and simulated LAI.
5、Missing limitations and methodological inconsistencies. The manuscript lacks any discussion of study limitations. Most critically, it appears that the authors use different land-use datasets for their analysis than the models they evaluate. They apply a cropland mask based on RESDC (1km resolution, lines 104-109) to define their study region, while TRENDY models use HYDE3.3 (0.5° resolution) for land-use forcing. Their own Figure 8 demonstrates these datasets disagree substantially in both spatial patterns and temporal dynamics. Yet the authors criticize TRENDY for using HYDE (lines 249-254) but do not acknowledge that comparing model outputs forced with one land-use dataset against observations masked with another is an inconsistency. Additional unacknowledged limitations include: (i) scale mismatch and homogeneity assumptions—while the authors note that 0.5° grid cells may obscure dynamics (line 255), they apply this only as a model limitation without acknowledging that their own analysis treats aggregated 0.5° cells as homogeneous cropland; (ii) lack of explanation of aggregation methods (see major comment 4); (iii) no consideration of alternative explanations for model-data (beyond lack of bimodal pattern) mismatch beyond missing double-cropping (e.g., incorrect phenology parameters, cultivar choices, or sowing dates that could be corrected without implementing full double- cropping). In my opinion a limitations section is needed to address these or other issues. It would also be interesting to test whether using HYDE-based cropland masks changes the observed bimodal pattern in remote sensing data. This would give insight on how much the land-use dataset inconsistency affects the main conclusions.
Response
We greatly appreciate the reviewer’s comments, as the land cover mask has always been one of the sources of error. We will first discuss the logic of our analysis and then make the corresponding modifications based on the reviewer’s suggestions.
In our analysis, we used the RESDC data as the true value, which was developed specifically for China and is widely applied. Indeed, there are certain discrepancies between the RESDC and HYDE data. Therefore, our analysis logic is as follows:
Examining the difference between remote sensing observations and simulations on actual cropland. This introduces two potential uncertainties: first, the inconsistency between the model’s cropland mask and the actual land cover; second, the mixed pixel issue at the 0.5° resolution, where pixels are not purely cropland, as shown in Figure 8.
Let’s first address the mixed pixel issue. At this resolution, mixed pixels are inevitable, and we can only determine whether a pixel is cropland based on a certain proportion threshold. We chose 50%, and the bimodal structure also indicates that the dominant signal is cropland, with no such signal for natural vegetation.
Next, we compared the 0.5° mask of RESDC and HYDE with the 50% threshold. As shown in the figure below, the mask ranges of both datasets are relatively consistent, with the differences being smaller than the total cropland area. This is because the proportion of cropland in the 0.5° grid point of HYDE is smaller than in the RESDC data. Further analysis also indicated that the results did not show significant changes, as shown in the results figure below.
Given the limited potential impact of HYDE, we have revised the discussion section as follows: we suggest removing the following sentence:
"Inappropriate parameterizations may also lead to systematic overestimation of grid-scale LAI values."
The following content has been revised:Change "Moreover, the TRENDY project employs the HYDE global historical environment database (Klein Goldewijk et al., 2017) as a proxy for cropland dynamics. Yet, while global products are useful at large scales, regional-scale land use/cover change (LUCC) datasets are often more accurate. The RESDC LUCC dataset, derived from remote sensing and validated at local scales, provides a more realistic representation of land cover in the Huang-Huai-Hai Plain. A comparison of HYDE3.3 and RESDC (Fig.8) shows that HYDE unrealistically exaggerates interannual variability in cropland area, despite the relative stability of land use in this region, and that its spatial distribution of croplands deviates from actual conditions." to "Moreover, the TRENDY project uses the HYDE global historical environment database (Klein Goldewijk et al., 2017) as a proxy for cropland dynamics. In contrast, we used the RESDC data, which is more widely applied in China, for the actual farmland coverage analysis. There are certain discrepancies between the two datasets, as shown in Figure 8. Although land use in this region is relatively stable, HYDE exaggerates unrealistic interannual variability in cropland area and its spatial distribution of croplands deviates from actual conditions. Both datasets face the mixed pixel problem at a 0.5° resolution, so a threshold is needed for analysis. We used a 50% cropland proportion as the threshold. At this threshold, the spatial distribution of both datasets at 0.5° resolution becomes more consistent, as the actual cropland proportion in the coarse-resolution pixels is higher in the RESDC data. We also analyzed the results under the HYDE mask, and the findings showed no significant changes."
At the same time, the paper focuses more on the impact brought about by multiple cropping information, so we have removed the following paragraph. Although the meaning is correct, it is not directly related to the issue addressed in our results: “To improve the accuracy and applicability of DGVMs, future research should extend analyses to larger regions to investigate double-cropping and fallow systems at the global scale, with a particular focus on three priorities: (1) incorporating explicit mechanisms for cropping systems; (2) optimizing regional parameterizations; and (3) integrating locally validated LUCC and crop calendar datasets.”
Reference
[1] Piao S , Yin G , Tan J ,et al. Detection and attribution of vegetation greening trend in China over the last 30 years[J].Global Change Biology, 2015, 21(4).DOI:10.1111/gcb.12795.
[2] Zhu, Z., Piao, S., Myneni, R. B., Huang, M., Zeng, Z., Canadell, J. G., Ciais, P., Sitch, S., Friedlingstein, P., Arneth, A., Cao, C., Cheng, L., Kato, E., Koven, C., Li, Y., Lian, X., Liu, Y., Liu, R., Mao, J., Pan, Y., Peng, S., Peñuelas, J., Poulter, B., Pugh, T. A. M., Stocker, B. D., Viovy, N., Wang, X., Wang, Y., Xiao, Z., Yang, H., Zaehle, S., and Zeng, N.: Greening of the Earth and its drivers, Nat. Clim. Change, 6, 791–795, https://doi.org/10.1038/nclimate3004, 2016.
[3] Masson-Delmotte et al. 2021. Climate change 2021: the physical science basis. Contribution of working group I to the sixth assessment report of the intergovernmental panel on climate change, 2(1), 2391.
[4] Zhou S, Chen T, Zeng N, et al. The Impact of Cropland Abandonment of Post-Soviet Countries on the Terrestrial Carbon Cycle Based on Optimizing the Cropland Distribution Map[J]. Biology, 2022, 11(5): 620.
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AC5: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC5 -
AC11: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC11
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AC1: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
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RC2: 'Comment on egusphere-2025-4997', Anonymous Referee #2, 25 Feb 2026
This paper compares LAI outputs from seven TRENDY DGVMs against three remote sensing products over the Huang-Huai-Hai Plain, a major double-cropping region in eastern China. The authors find that remote sensing consistently reveals a bimodal seasonal LAI cycle (peaks in April and August, corresponding to winter wheat and summer maize), whereas none of the DGVMs reproduce this pattern. They also report that DGVMs tend to overestimate LAI magnitude and underestimate the cropland contribution to regional greening. The paper calls for incorporating explicit double-cropping mechanisms into DGVMs.
I appreciate the authors' effort to draw attention to the limitations of current DGVMs in representing intensively managed croplands. This is an important and, I think, underappreciated problem, particularly as we increasingly rely on these models for carbon budget attribution and greening studies. The Huang-Huai-Hai Plain is a well-chosen study area, and the use of multiple remote sensing products alongside multiple models adds robustness. I do think the core message of this paper is worth communicating. But at the same time, I do have several concerns that prevent the paper from reaching its potential in its current form.
First of all, the introduction needs substantial restructuring. As it stands, the logic chain is fragmented and the narrative wanders through several loosely connected themes without building a coherent argument toward the study's objective. The introduction opens with a broad discussion of vegetation change, greening, and remote sensing (L23–33), which is fine as context-setting. But then it takes a detour into the specific quantitative findings of Zhu et al. (2016) — reporting that 25–50% of vegetated land shows increased LAI, that CO₂ accounts for 70% of greening, nitrogen deposition 9%, and so on (L36–41). This level of numerical detail belongs in the Discussion when interpreting your own results, not in the Introduction. The important point from that work — that DGVMs attribute most greening to CO₂ fertilisation — can be stated in one sentence. The transition at line 42 ("However, managed lands—particularly croplands—have been shown by observations to make a substantial contribution to global greening") is actually the key motivating observation for the study, but it is buried rather than highlighted. And then the transition at line 47 is jarring: the paper suddenly shifts from "croplands challenge DGVM greening attribution" to "it is essential to first validate that DGVMs can accurately capture the fundamental seasonal characteristics of vegetation." The logical connection — that if DGVMs get the seasonal cycle of croplands wrong, their estimates of cropland productivity and greening contribution are unreliable — is never stated. The reader has to infer it. Lines 47–52 then discuss phenology in quite general terms (SOS advancement, EOS delay, peak greenness enhancement, global warming and northern ecosystem productivity), which reads like textbook material that does not connect specifically to the problem of double-cropping. By the time the reader reaches the study objective at line 68, they have passed through global greening drivers, CO₂ fertilisation percentages, generic phenology concepts, and global multiple cropping statistics — none of which flow naturally into each other. I would suggest reorganising the introduction around a cleaner logic chain.
Moving to the core analysis, my main concern is that the paper stays largely at the descriptive level. The paper documents that models fail but does not explore why. Most TRENDY models were never designed to simulate double-cropping, so the mismatch is expected. This does not make the paper pointless as systematic documentation has value, but it needs a diagnostic dimension. I would suggest adding a table summarising each model's cropland representation (crop functional types, phenology scheme, management features, ability to simulate sequential cropping). This information is available from published model descriptions and would immediately contextualise the results. The three-type classification of seasonal patterns (L178–183) is interesting but should be linked to model design choices rather than left hanging. The Discussion similarly needs to move from restating results to interpreting them: which models already have infrastructure for double-cropping? What would need to change in the TRENDY protocol?
The land-use mask inconsistency is a real problem. The analysis uses RESDC (1 km) to define cropland, but TRENDY models are forced with HYDE3.3 (0.5°). Figure 8 shows these datasets disagree substantially. This means part of the model–observation mismatch could reflect differences in what land is classified as cropland, not just the absence of double-cropping mechanisms. A sensitivity test such as applying the HYDE mask to the remote sensing data and checking whether the bimodal pattern persists would resolve this. The HYDE data are already available to the authors from Figure 8, so this requires no new data.
Data processing methods are missing. The three remote sensing products have very different native resolutions and are all aggregated to 0.5°/monthly, but the aggregation procedure is not described. Monthly means vs. maxima, the order of masking vs. upscaling, and MODIS quality flag handling can all affect peak amplitude and timing — exactly what the paper analyses. A brief methods subsection would address this.
The manuscript is redundant in many sections. The same three conclusions appear at L215–222, in the Discussion, and in the Conclusions. The paragraph at L219–222 essentially repeats L215–218 with different wording. I would remove the end-of-Results summary entirely and add a Limitations subsection instead.
The greening trend analysis deserves more attention. This is arguably the most novel part of the paper. The finding that ISAM and LPJmL show browning where all observations show greening is striking, what might explain it? Even a tentative hypothesis based on published model descriptions would add value. The seasonal pattern of greening (strongest in spring, consistent with enhanced wheat productivity) could be connected more explicitly to agricultural drivers like cultivar change or fertilisation.
Specific Comments:
The section heading at L22 has a typo ("Introdution"). Missing spaces before parenthetical references occur throughout. The Figure 1 caption has a placeholder ("at xx resolution"). "LPX-Bern"/"LPXBern" is inconsistent. The second results subsection (L200) is mislabelled "3.2" instead of "3.3." "MOD15A12H" at L355 should be "MOD15A2H."
Figures 5 and 6 would benefit from a summary panel overlaying remote sensing curves with a model ensemble envelope.
Analysis code should be archived for reproducibility.
Citation: https://doi.org/10.5194/egusphere-2025-4997-RC2 -
AC12: 'Response of review2 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Response of review “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”
Dear Reviewer,
Thank you very much for your time and insightful suggestions. Your in-depth discussion has been especially valuable for improving this paper. We have also provided detailed responses to address your concerns. Although some of the results might be expected from a theoretical perspective, the goal of this paper is to quantify current deficiencies and thereby draw attention to the need for improving the representation of multi-cropping regions in DGVM development. This is of great importance for the advancement of Earth system models. Below are our point-by-point responses to your comments.
Thanks again.
Tiexi CHEN and co-authors
General remarks
This paper compares LAI outputs from seven TRENDY DGVMs against three remote sensing products over the Huang-Huai-Hai Plain, a major double-cropping region in eastern China. The authors find that remote sensing consistently reveals a bimodal seasonal LAI cycle (peaks in April and August, corresponding to winter wheat and summer maize), whereas none of the DGVMs reproduce this pattern. They also report that DGVMs tend to overestimate LAI magnitude and underestimate the cropland contribution to regional greening. The paper calls for incorporating explicit double-cropping mechanisms into DGVMs.
I appreciate the authors' effort to draw attention to the limitations of current DGVMs in representing intensively managed croplands. This is an important and, I think, underappreciated problem, particularly as we increasingly rely on these models for carbon budget attribution and greening studies. The Huang-Huai-Hai Plain is a well-chosen study area, and the use of multiple remote sensing products alongside multiple models adds robustness. I do think the core message of this paper is worth communicating. But at the same time, I do have several concerns that prevent the paper from reaching its potential in its current form.
Response
Thank you for your generally positive evaluation of our manuscript. We fully agree that this is an important and challenging issue.
On the one hand, Dynamic Global Vegetation Models (DGVMs) are powerful tools for identifying the drivers of global greening and attributing their relative contributions. On the other hand, current DGVMs still lack adequate representation of managed lands, particularly in regions characterized by intensive agricultural practices such as double-cropping systems. In situations where discrepancies arise among model outputs, comparative or ensemble-based analyses are commonly adopted; however, rigorous performance evaluation against observations remains essential.
With the increasing global demand for food, cropping intensity has risen substantially through multiple-cropping practices, among which double-cropping plays a crucial role. It accounts for approximately 17.42% (2.62 × 10⁶ km²) of global cropland area (Zhang et al., 2021), and therefore cannot be neglected in large-scale assessments.
Why, then, has limited progress been made in addressing this model deficiency? We argue that one key reason is the lack of broad consensus within the research community regarding the magnitude and implications of this issue. This gap highlights the need for systematic case studies in representative regions to explicitly quantify its impacts.
In this study, although we are unable to fully disentangle all underlying processes across the seven DGVMs analyzed, we aim to clearly demonstrate the significant biases associated with the absence of double-cropping representations. This is achieved by quantifying discrepancies between remote sensing observations and model simulations. More importantly, we hope this work will help raise awareness among model developers and stimulate future improvements in the representation of agricultural management processes.
Major comments
First of all, the introduction needs substantial restructuring. As it stands, the logic chain is fragmented and the narrative wanders through several loosely connected themes without building a coherent argument toward the study's objective. The introduction opens with a broad discussion of vegetation change, greening, and remote sensing (L23–33), which is fine as context-setting. But then it takes a detour into the specific quantitative findings of Zhu et al. (2016) — reporting that 25–50% of vegetated land shows increased LAI, that CO₂ accounts for 70% of greening, nitrogen deposition 9%, and so on (L36–41). This level of numerical detail belongs in the Discussion when interpreting your own results, not in the Introduction. The important point from that work — that DGVMs attribute most greening to CO₂ fertilisation — can be stated in one sentence. The transition at line 42 ("However, managed lands—particularly croplands—have been shown by observations to make a substantial contribution to global greening") is actually the key motivating observation for the study, but it is buried rather than highlighted. And then the transition at line 47 is jarring: the paper suddenly shifts from "croplands challenge DGVM greening attribution" to "it is essential to first validate that DGVMs can accurately capture the fundamental seasonal characteristics of vegetation." The logical connection — that if DGVMs get the seasonal cycle of croplands wrong, their estimates of cropland productivity and greening contribution are unreliable — is never stated. The reader has to infer it. Lines 47–52 then discuss phenology in quite general terms (SOS advancement, EOS delay, peak greenness enhancement, global warming and northern ecosystem productivity), which reads like textbook material that does not connect specifically to the problem of double-cropping. By the time the reader reaches the study objective at line 68, they have passed through global greening drivers, CO₂ fertilisation percentages, generic phenology concepts, and global multiple cropping statistics — none of which flow naturally into each other. I would suggest reorganising the introduction around a cleaner logic chain.
Response
Thank you very much for your insightful comments. We recognize that the lack of a clear logical structure in the Introduction has led to confusion, including Reviewer 1’s concern regarding the scientific significance of this study.
To better highlight the core research question, we have substantially condensed the Introduction and clarified its logical flow. Specifically, we now emphasize that, given the strong reliance of current research on DGVMs as a powerful tool, and the substantial contribution of croplands to global greening, it is essential to rigorously evaluate the ability of DGVMs to simulate vegetation dynamics at the regional scale.
The revised Introduction is provided below:
Introduction
Vegetation change and its climatic feedback are central to current global change research, as terrestrial ecosystems remain highly sensitive to anthropogenic and natural drivers (Houghton, 1995; Esau et al., 2016). Over recent decades, a significant global "greening" trend—characterized by an interannual increase in leaf area index (LAI) or greenness—has been widely documented through satellite-based observations (Myneni et al., 1997; Huete et al., 2002; Piao et al., 2019). To attribute these changes, Dynamic Global Vegetation Models (DGVMs) have become indispensable tools, generally identifying the CO₂ fertilization effect as the primary driver of global vegetation growth (Zhu et al., 2016; Keenan et al., 2013).
However, a significant discrepancy exists between model attributions and observational evidence regarding managed lands. While DGVMs emphasize CO₂ fertilization (Zhu et al., 2016), recent remote sensing studies highlight that intensive land management, particularly in croplands, contributes substantially to global greening. For instance, the greening observed in China and India is predominantly driven by agricultural intensification rather than natural factors (Chen et al., 2019). This contradiction suggests that current DGVMs may overestimate the role of CO₂ while underrepresenting the impact of human-induced agricultural dynamics, highlighting an urgent need to evaluate and refine how models simulate agricultural systems.
The reliability of long-term greening attributions in DGVMs depends fundamentally on their ability to capture short-term seasonal dynamics. If a model cannot accurately simulate the seasonal cycle of vegetation—including phenological shifts and peak productivity—its estimates of cumulative biomass and long-term trends remain questionable. While natural vegetation adapts to climate change through physiological adjustments (Huang et al., 2017), croplands exhibit unique phenological traits dictated by human management. This is most evident in regions characterized by multiple cropping systems, where intensive agricultural activities create complex seasonal patterns—such as multiple greenness peaks—that differ starkly from the unimodal cycles of natural ecosystems.
Despite the fact that multiple cropping systems cover approximately 12% of global croplands and are vital for cereal production (Waha et al., 2020; Wu et al., 2018), these processes are rarely or inadequately represented in current DGVMs. Most models simplify agricultural land use or fail to account for the intermittent fallow periods and shifting cultivation intensities inherent in these systems (Liu, 2021). Consequently, there is a critical knowledge gap in whether DGVMs can accurately replicate the intensified seasonality of highly managed landscapes. In this study, we focus on the Huang-Huai-Hai Plain, a representative region dominated by a stable winter wheat–summer crop double-cropping system since the 1980s. The objective of this research is to evaluate the capacity of state-of-the-art DGVMs to simulate the vegetation seasonality driven by intensive double-cropping, thereby identifying the specific structural limitations of these models in representing human-managed ecosystems.
Moving to the core analysis, my main concern is that the paper stays largely at the descriptive level. The paper documents that models fail but does not explore why. Most TRENDY models were never designed to simulate double-cropping, so the mismatch is expected. This does not make the paper pointless as systematic documentation has value, but it needs a diagnostic dimension. I would suggest adding a table summarising each model's cropland representation (crop functional types, phenology scheme, management features, ability to simulate sequential cropping). This information is available from published model descriptions and would immediately contextualise the results. The three-type classification of seasonal patterns (L178–183) is interesting but should be linked to model design choices rather than left hanging. The Discussion similarly needs to move from restating results to interpreting them: which models already have infrastructure for double-cropping? What would need to change in the TRENDY protocol?
Response
We agree with the reviewer’s professional judgment that the core analysis in the original manuscript remains largely at the descriptive level of model-observation mismatches, without in-depth exploration of the model structural causes underlying the biases, resulting in a lack of diagnostic value and mechanistic interpretation of the study. Although most models in the TRENDY ensemble were not originally designed to incorporate double-cropping simulation modules, and this mismatch is to a certain extent expected, the systematic diagnosis of such biases is precisely the core academic value that this study should supplement. In the revised manuscript, we will upgrade the analytical content from three dimensions:
First, we will add a table to systematically summarize the core structural characteristics of the 7 models used in this study, specifically including the classification scheme of crop functional types, phenology simulation schemes, agricultural management module settings, and the capability to simulate sequential cropping and double-cropping. All information will be derived from the official published description documents of each model, to provide complete structural background support for the interpretation of the results.
Second, we will establish the correlation between simulation results and model design choices, conduct a corresponding analysis between the three-type classification of LAI seasonal patterns in the original manuscript and model structural characteristics, and clarify the intrinsic relationship between the seasonal simulation bias characteristics of different models and their phenology schemes and cropland management representation capabilities, thus achieving the upgrade from "describing bias phenomena" to "interpreting the causes of biases".
Third, we will comprehensively restructure the Discussion section, abandon repetitive restatements of the results, and focus on the mechanistic interpretation of three core issues: which models already have the basic framework for double-cropping simulation, and the core reasons why this function is not activated under the TRENDY protocol; the core adjustments needed in the model structure and simulation protocol of the TRENDY multi-model ensemble for regional cropland simulation; and the cascading effects of the lack of double-cropping mechanisms on DGVM simulations of regional carbon cycles and climate feedbacks. This will echo the scientific questions raised in the introduction and strengthen the scientific significance of the study.
Table 3. Overview of the simulation capabilities for Cropland of the selected models from Trendy v12
Dataset Name
Cropland module
Crop Functional Type
Phenology
Irrigation module
Fertilization Module
Single/multiple cropping
ED
NAN
ISAM
YES
Maize (C4)、Wheat、Rice、Soybean(C3)
Defined by accumulated temperature
YES
YES
Single
LPJ-GUESS
YES
Separate crop phenology schemes on a daily time-step are present for simulations with and without N-limitation. Cropland without N-limitation is represented by eleven crop PFTs (temperate cereals, rapeseed, pulses, sugarbeet, maize, soybean, tropical cereals, sunflower, peanut, cassava and rice), simulated separately (without inter-PFT competition) and two grass PFTs (competing C3 and C4 grass) as cover crop between harvest and sowing. The same grass PFTs are used to represent pastures. Currently, two crop PFTs are defined for N-limited simulations (wheat and maize).
Defined by accumulated temperature and precipitation
YES
YES
Single
LPJml
YES
In LPJmL4, 12 different annual CFTs are simulated (Table S10), similar to Bondeau et al. (2007)
with the addition of sugar cane. The basic idea of CFTs
is that these are parameterized as one specific representative crop (e.g. wheat, Triticum aestivum L.) to represent a broader group of similar crops (e.g. temperate cereals)
The phenological development of crops in LPJmL4 is driven by temperature through the accumulation of growing degree days and can be modified by vernalization requirements and sensitivity to daylength (photoperiod) for some CFTs and some varieties.
YES
YES
Single
LPXbern
YES
The farmland and the pasture share the common herbaceous PFT, without distinguishing specific crop types such as wheat, corn, or rice, and there is no dedicated crop PFT.
The core physiological process framework is consistent with the natural herbal PFT.
NAN
YES
Single
ORCHIDEE
YES
Define two specific agricultural PFTs: Agricultural C3 grass and Agricultural C4 grass
ORCHIDEE assumes
that all C3 agriculture is a perennial prairie and does not
account for harvest.
NAN
NAN
Single
VISIT
YES
The global farmland is divided into three core functional types:
1.C3 crop type, represented by crops such as wheat, which adopts the parameterization scheme of C3 plant photosynthetic physiology;
2. C4 crop type, represented by crops such as corn in tropical/subtropical regions, which is adapted to the photosynthetic and water utilization characteristics of C4 plants;
3.Rice field type specifically designed for the rice-growing areas in the Asian monsoon region. In addition to the basic crop physiological simulation, it additionally couples the seasonal flooding hydrological process and the exclusive module for rice field CH₄ emissions.
In response to the agricultural production characteristics of different climate zones, differential planting systems and phenological-driven schemes are adopted. The core rules are as follows:
1. In temperate regions: A one-year cropping system is implemented, with the growth cycle driven by temperature thresholds:
◦ The core indicators for initiating and ending the growing season are the monthly average temperature of 5°C as the critical value;
◦ When the growth season begins, a fixed amount of carbon is added to the crop biomass reservoir to simulate the initialization process of sowing/transplanting;
◦ When the surface temperature is below the critical value of 5°C, the crop harvest process is triggered.
2. In tropical regions (average annual temperature > 20°C): A continuous annual cropping system is adopted, without setting seasonal start and end periods for growth. Sowing and harvest occur continuously at a constant rate each month.
NAN
NAN
Single
The land-use mask inconsistency is a real problem. The analysis uses RESDC (1 km) to define cropland, but TRENDY models are forced with HYDE3.3 (0.5°). Figure 8 shows these datasets disagree substantially. This means part of the model–observation mismatch could reflect differences in what land is classified as cropland, not just the absence of double-cropping mechanisms. A sensitivity test such as applying the HYDE mask to the remote sensing data and checking whether the bimodal pattern persists would resolve this. The HYDE data are already available to the authors from Figure 8, so this requires no new data.
Response
We acknowledge that the original manuscript failed to fully disclose the application differences between the RESDC and HYDE3.3 land use datasets, nor did it verify the potential impact of such differences on the core conclusions, which constitutes an omission in methodological rigor. In the revised manuscript, we will strictly follow your suggestions to complete two core revisions and supplementary analyses:
On the one hand, we will supplement a sensitivity test of the land use mask. Using the HYDE3.3 0.5° cropland mask, which is fully consistent with the forcing data of the TRENDY models, we will re-perform mask extraction and spatiotemporal change analysis for both remote sensing and simulated LAI data. We will systematically compare the differences in the bimodal seasonal characteristics of LAI and interannual greening trends derived from remote sensing data under the two cropland masks, quantify the contribution of inconsistent cropland classification standards to the model-observation mismatch, and verify the robustness of the core conclusions of this study. The relevant results will be supplemented to the Results section of the main text, and the corresponding figures will be included in the supplementary materials.
On the other hand, we will clearly define the application boundaries and applicable scenarios of the two datasets in the Methods section. We will clarify that HYDE3.3 is the official global-scale land use forcing data adopted by the TRENDY models, while RESDC is a regional-scale remote sensing-based land cover product that is more consistent with the actual spatial distribution of croplands in the Huang-Huai-Hai Plain. Meanwhile, we will objectively describe the advantages and limitations of the two datasets, revise the one-sided statements about the HYDE dataset in the original manuscript, and resolve the issue of inconsistent methodological descriptions.
Figure 1-3 is provided in the supplementary materials.
Mask contrast and sensitivity tests revealed that differences in the Cropland masks produced by the two datasets are very small, and they do not have a significant impact on the bimodal structure of LAI in the farmland. We believe that the mask is not the cause of the seasonal differences in remote sensing and simulated LAI.
Data processing methods are missing. The three remote sensing products have very different native resolutions and are all aggregated to 0.5°/monthly, but the aggregation procedure is not described. Monthly means vs. maxima, the order of masking vs. upscaling, and MODIS quality flag handling can all affect peak amplitude and timing — exactly what the paper analyses. A brief methods subsection would address this.
Response
We acknowledge that the comprehensive disclosure of the entire data processing workflow is a fundamental prerequisite for ensuring the reproducibility of research results and the reliability of conclusions; we sincerely apologize for the significant lack of detail regarding the aggregation and quality control procedures for multi-source remote sensing data in the initial version of this manuscript. In this revision, we will introduce a dedicated subsection titled "Spatio-temporal Aggregation and Standardization of Multi-source Data" within Section 2.2 (Remote Sensing Data) of the paper to provide a complete and lucid account of the entire processing workflow,which clarifies the operational details for the three core questions raised by the reviewer one by one to ensure full reproducibility of the method:
Temporal aggregation method: For the 8-day resolution data from MODIS and GLASS, we first performed linear interpolation to daily resolution, and then calculated the arithmetic mean of all valid daily observations within each calendar month to derive the monthly LAI value. For the semi-monthly resolution GIMMS data, the monthly LAI value was represented by the arithmetic mean of the first and second half-month observations in the same month.
This method can smooth the random noise of single-period data while fully retaining the characteristic bimodal seasonal dynamics of the double-cropping system, and avoids the over-amplification of transition period signals caused by the maximum value composite method.
Spatial aggregation method: For the high-resolution raw data of MODIS (500 m) and GLASS (0.05°), the area-weighted averaging method was used to aggregate the data to the target 0.5° grid, rather than simple arithmetic averaging. This method eliminates the bias caused by the pixel area proportion of different resolution data, and ensures that the value of the 0.5° grid fully represents the mean cropland LAI of the corresponding region, which is completely matched with the grid scale of the TRENDY model outputs.
Implementation sequence of cropland masking: We adopted the workflow of aggregation followed by cropland masking. Mixed pixels are an unavoidable issue in scale conversion. It is difficult to find 0.5° grids with pure cropland cover in both model results and real-world remote sensing images. We therefore performed grid screening based on the 0.5° aggregated land use/cover percentage data. A grid was classified as a cropland grid in a given year when its cropland coverage exceeded 50%. If the grid was consistently classified as cropland throughout the study period, we considered it to have stable land use with no conversion, and included it in the cropland mask.
Through this method, we aim to extract the seasonal characteristics of croplands while retaining sufficient sample representativeness and preserving cropland information to the greatest extent possible. This workflow is applicable to both the RESDC land cover dataset and the HYDE land use dataset. We have also included the masking results based on the HYDE dataset in the Discussion section as a sensitivity analysis to test whether the HYDE-based cropland mask alters the observed bimodal pattern in the remote sensing data.
The manuscript is redundant in many sections. The same three conclusions appear at L215–222, in the Discussion, and in the Conclusions. The paragraph at L219–222 essentially repeats L215–218 with different wording. I would remove the end-of-Results summary entirely and add a Limitations subsection instead.
Response
We agree with the reviewer’s suggestions that the original manuscript has issues of repetitive expression of core conclusions and content redundancy, and lacks the discussion of study limitations, which is essential for academic papers and does not comply with the academic norms of international journals. In the revised manuscript, we will complete two core revisions:
First, we will thoroughly streamline the redundant content of the manuscript, delete the repetitive summary paragraphs at the end of the Results section, condense the expression in the Discussion and Conclusion sections, and remove content with synonymous repetition. We will achieve a structural division where the Results section only presents objective analysis results, the Discussion section focuses on mechanistic interpretation, and the Conclusion section extracts core scientific findings and research prospects, ensuring that the three sections perform their respective functions without overlapping or redundant content.
Second, we will add an independent subsection entitled Study Limitations at the end of the Discussion section, to comprehensively and objectively disclose the core limitations of this study, specifically including the potential biases from the selection of land use datasets, the scale matching issue of the 0.5° grid, other potential influencing factors for model-observation mismatches, and the limitations of extrapolating the findings from the study region to other areas. This will ensure that the expression of the study conclusions is objective and rigorous.
The greening trend analysis deserves more attention. This is arguably the most novel part of the paper. The finding that ISAM and LPJmL show browning where all observations show greening is striking, what might explain it? Even a tentative hypothesis based on published model descriptions would add value. The seasonal pattern of greening (strongest in spring, consistent with enhanced wheat productivity) could be connected more explicitly to agricultural drivers like cultivar change or fertilization.
Response
We sincerely thank the reviewer for recognizing the research value of the greening trend analysis section. The original manuscript had insufficient in-depth exploration and elaboration of this part, and failed to fully release the innovative value of the study. In the revised manuscript, we will focus on deepening the analytical content of this section, and specifically supplement two core modules:
First, we will systematically analyze the potential causes of divergent greening trends among models. Based on the official published description literature of each model, we will put forward mechanistic tentative hypotheses for the browning trends simulated by the ISAM and LPJmL models, which are completely opposite to the greening signals observed in all remote sensing products. We will focus on comparing the core differences between these two models and other models in four dimensions: the parameterization scheme of crop CO₂ fertilization effects, the design of cropland phenology modules, the representation of nitrogen cycle processes, and the representation of agricultural management measures. We will systematically analyze the potential driving mechanisms of the simulated browning trends, filling the gap in the original manuscript where only the phenomenon was described without exploring the causes.
Second, we will establish the correlation between the seasonal characteristics of greening trends and regional agricultural driving factors. We will link the finding of "the strongest greening trend in spring" in this study to the changes in agricultural management practices in the main winter wheat producing areas of the Huang-Huai-Hai Plain, supplement empirical data and literature support on agricultural driving factors in the region including crop variety improvement, increased fertilizer application, irrigation management adjustment, and agricultural machinery application, interpret the contribution of agricultural management measures to regional cropland greening, and improve the regional pertinence and mechanistic explanatory power of the analysis.
Specific Comments:
The section heading at L22 has a typo ("Introdution"). Missing spaces before parenthetical references occur throughout. The Figure 1 caption has a placeholder ("at xx resolution"). "LPX-Bern"/"LPXBern" is inconsistent. The second results subsection (L200) is mislabelled "3.2" instead of "3.3." "MOD15A12H" at L355 should be "MOD15A2H".
Response
For the detailed issues of format, spelling, and terminology consistency throughout the manuscript pointed out by the reviewer, we will complete a comprehensive and item-by-item revision in the modified manuscript, which specifically includes: correcting the typo in the section heading, changing "Introdution" to "Introduction"; uniformly revising the formatting issue of missing spaces before parenthetical references throughout the manuscript, in strict compliance with the citation format specifications of the target journal; revising the placeholder in the caption of Figure 1, and supplementing the native resolution information of the remote sensing products; unifying the nomenclature of the model name throughout the manuscript, standardizing it as "LPX-Bern" to eliminate the inconsistency in abbreviation; correcting the numbering error of the subsection heading in the Results section, changing "3.2" at line 200 to "3.3"; correcting the typo of the remote sensing product name, changing "MOD15A12H" to "MOD15A2H". Meanwhile, we will complete a full read-through and check of the entire manuscript to eliminate all detailed errors in spelling, punctuation, and formatting, to ensure the academic standardization of the manuscript.
Figures 5 and 6 would benefit from a summary panel overlaying remote sensing curves with a model ensemble envelope.
Analysis code should be archived for reproducibility.
Response
In response to your suggestions regarding the figures, we will optimize the visualization of Figures 5 and 6 in the revised manuscript. Meanwhile, we will introduce a summary panel that overlays the mean curves and upper and lower envelopes of both the multi-source remote sensing LAI data and the TRENDY model ensemble. This approach will intuitively illustrate the overall characteristics of the discrepancies between the models and observations, thereby enhancing the information density and readability of the figures and enabling readers to quickly grasp the core results.
Figure 4 is provided in the supplementary materials.
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AC12: 'Response of review2 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
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AC2: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC2 -
AC3: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC3 -
AC4: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC4 -
AC6: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC6 -
AC7: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC7 -
AC8: 'Response of review1 “Seasonal Cycle Biases in DGVM Simulations of Double- Cropping Systems: A Case Study in the Huang-Huai-Hai Plain”', Tiexi Chen, 13 Apr 2026
Publisher’s note: this comment is a copy of AC1 and its content was therefore removed on 14 April 2026.
Citation: https://doi.org/10.5194/egusphere-2025-4997-AC8
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View my comments in the attached file.