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Review

Predictive Production Models for Mountain Meadows: A Review

Departamento de Ciencias Agrarias y del Medio Natural, Escuela Politécnica Superior, Universidad de Zaragoza, Ctra Cuarte s/n, 22071 Huesca, Spain
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Author to whom correspondence should be addressed.
Agronomy 2024, 14(4), 830; https://doi.org/10.3390/agronomy14040830
Submission received: 20 March 2024 / Revised: 15 April 2024 / Accepted: 15 April 2024 / Published: 17 April 2024

Abstract

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Meadows are the most important source of feed for extensive livestock farming in mountainous conditions, as well as providing many environmental services. The actual socioeconomic situation and climate change risk its conservation. That is why finding its optimal management is important. To do so, predictive models are a useful tool to determine the impact of different practices and estimate the consequences of future scenarios. Empirical models are a good analytical tool, but their applications in the future are limited. Dynamic models can better estimate the consequences of newer scenarios, but even if there are many dynamic models, their adaptation into grassland production estimation is scarce. This article reviews the most suitable predictive models for grass production in mountain meadows when data on agricultural management (mowing, grazing, fertilization) and forage value are available, considering the conservation of plant biodiversity.

1. Introduction

Traditional livestock farming in mountainous areas is strongly dependent on hay meadows [1]. These meadows are communities formed by different plant species from different botanical families that grow together as a single crop. On those farms, meadows are cut during the summer, and if the summer is wet enough, they can be cut a second time. They are also used for grazing in spring and autumn. That is why they constitute the keystone of traditional livestock farming [2,3,4].
Not only do they help farmers meet their feeding needs, but they also provide environmental services. Due to their dynamics, meadows can act as carbon and nitrogen sinks by capturing those elements into organic matter in the soil, helping in climate change mitigation [5,6]. They are an important biodiversity reservoir, providing adequate ecological niches for many plants and animals [7,8]. Lastly, it should be noted the great landscape value that they have, making the rural environment more bucolic [9].
Those services can be affected by changes in management. Given the actual climatic conditions, where heat stress days and drought days are increasing, meadows can pivot from being a carbon sink into a carbon emitter, especially if they are heavily fertilized or if there is overgrazing [5].
System biodiversity is also driven by management practices, mainly mowing, grazing, and fertilization [10]. If there are changes in those practices, be they in excess or absent, there will be changes in vegetation dynamics, species distribution, and landscape biodiversity [8].
Meadows are a more complex crop system than conventional monocultures [11]. Instead of having a single species, we have a community formed not only by different species but also by different botanical families, each one behaving and responding differently to farm management and climatic conditions [12]. Given that complexity, it is difficult to establish which practices are beneficial for the whole meadow. For example, nitrogen fertilization would be beneficial for grasses but detrimental for legumes [8]. On the other hand, biodiversity gives meadows a higher resiliency, adapting better to stressful situations like floods, heat stress, or drought [13].
Abandonment of traditional livestock farming, especially in disadvantaged areas like mountainous areas, has been a constant issue since the 1980s, leading to a decrease in meadow area [2]. Although biodiversity usually increases right after meadow abandonment, in the long term, it will be significantly lower than it was when it was managed [14]. Intensification of production also decreases biodiversity due to the higher fertilization rates and the increase in grazing days [14,15].
In order to preserve meadows and maintain the ecosystemic services they bring, their management must be profitable [16]. Finding a balance between profit and conserving biodiversity while adapting to climate change is quite a challenge [17,18]. Actually, permanent grasslands in Europe occupy 33% of the agricultural area, or about 56.9 Mha (https://ec.europa.eu/eurostat/data/database, accessed on 9 April 2024).
During the past four years, the production, forage quality, and floristic diversity of several hay meadows in the Aragonese Pyrenees have been quantified. Agricultural management practices and meteorological variables have also been recorded during this period. With this information, we intend to calibrate a prediction model that will allow us to evaluate the production–conservation binomial of these meadows in the future under different management.
Therefore, a literature review of the use of models in different types of grasslands and productive environments is carried out, with special emphasis on the quantity and quality of the data necessary for their application. It also considers the way in which agrarian management is treated, namely, the quantity and timing of cuttings and grazing, the type and quantity of fertilization, etc. Finally, consideration is given to the way in which such models value changes in plant biodiversity in these systems.

2. Crop Predictive Models

Meadow profitability can be improved by optimizing farm management by adjusting fertilizing rates, mowing times, and grazing days. But knowing how to adjust those practices is quite difficult; it would take thorough research for each practice on each meadow to measure the impact of each practice. To facilitate this enormous task, there are predictive models that allow us to infer the impact of different practices and scenarios on production [19].
Predictive models allow us to precisely predict crop reality given specific management, soil, and climatic conditions at various temporal resolutions [20]. They are able to simulate the entire field situation by using relatively little field data [19].
Predictive models are mathematical approximations of the phenomena that happen in the atmosphere–plant–soil system, integrating all natural processes that influence these phenomena [21]. Each model uses a different mathematical approximation because there are different hypotheses in the different fields of study for the different natural processes. Usually, those approximations have no linear dependence on each other, which leads to important changes in the results with minimum changes in the input [21]. But it is important to be precise about what we want to predict and what the specific model requirements are [17].
They suppose a handy tool to analyze different scenarios given hypothetical situations and to know the previsible impact that those changes determined in the hypothesis will have on the modeled parameters [13,21,22].
One of their main uses is food security [23]. Because it allows us to predict the amount of food that will be available. That is especially useful with the current climate change situation. Despite the uncertainty of how the climate in the future will be, using predictive models, we can estimate the impact of long heat waves, droughts, etc. that are previsible to be more frequent [24].
We can classify predictive models according to their type as follows: they can be empirical (static), or they can be dynamic.
Empirical models are only built based on field data. They are statistical constructions to explain data variability given determined conditions at a specific moment. Usually, they are based on regressions, and although they are useful to describe and analyze, they cannot make predictions outside the field data range. The extrapolation of the result is at least very speculative [25].
On the other hand, dynamic models are based both on field data and equations that represent natural processes. They are more complex to parametrize and validate, but at the same time, they can be used for more situations than the empirical models [25].
We can also look at the complexity of the model; as the model gets more complex, it will better explain the entity and be more robust. But as a consequence, analyzing the impact of the different factors will be more difficult; there will be more correlations between parameters, and there will be a higher demand for calibration and validation [21,26].
On the contrary, as the model gets simpler, it will be easier to evaluate the impact of each factor, there will be less correlation between parameters, and validation and calibration will be simpler. But as a consequence, the model will be less robust, and there will be more differences between observed values and predicted values [21,26].
The area of application is one of the major drivers of complexity. Globalist models can be applied to many different situations, but they are more complex than other models that are more local [17].
There is a need to find a balance between explaining variability properly and having a manageable number of variables. If we use many variables, the model can get so complex that it will require enormous computing power to run simulations [27].
In our case of study, that is, meadows, there are specific parameters that should be considered that are not necessary for other crops. As meadows are used for animal feed, it is important to know what the impact on nutritional value will be. There are many factors that affect it, such as the diversity of species, which will change its nutritional value depending on the species that it contains and the quantity in which they are present [25]. Phenology will also play a key role in nutritional value because, as phenology advances, digestibility will decrease [28]. In addition, fertilization will be another factor that will affect nutritional value, especially nitrogen fertilization [28].
The impact of each factor will be different than in conventional crops, with biodiversity having one of the highest impacts [29]. But other parameters, like carbon, will have different impacts depending on the diversity of species [14].
Meadow management is also more complex than the management of other crops. There is a need to take into account practices like mowing or grazing, which implies that there is more than one type of harvest and more than one harvest per year, in contrast with other crops where there is only one harvest per year [13]. Current developments in remote sensing open new opportunities to measure objectively more parameters at a relatively low cost [30,31].

2.1. Empirical Models

This type of model is mainly used to describe and analyze observed situations. But there are studies where they have to infer conclusions based on the empirical model [32].
They can properly determine tendencies within actual management under actual practices, given that information is available to predict results within those conditions [33]. But the main purpose of the study must be clear, because depending on the goal, different types of results will be needed, and as a consequence, there will be certain statistical tools [34]. It is important not to try to infer conclusions outside of the range of field data due to the uncertainty outside this range [35].
Many empirical models are based on remote sensing. This is a cost-effective technique to get data objectively, and that is why it is widely used [36,37]. Most of them use the Normalized Vegetation Index (NDVI) to determine the amount of biomass present in the meadow [38]. Many of them are based on satellite imagery, which has the drawback of having low resolution, and as a result, it can only be successfully used when the area is large and homogenous [39]. In order to improve resolution, there are studies that use Unmanned Aerial Vehicles (UAV), and in these cases, small fields with higher heterogeneity can be studied [40]. Another remote sensing technique that has been applied to build empirical models is Lidar. This technology allows for the creation of a three-dimensional map from which it is possible to calculate biomass volume. Although it is considered a promising technology, its cost is still too high [41].
Recently, the development of friendly use of new Artificial Intelligence (AI) techniques has allowed us to let them use them in crop modeling [42]. There are many AI tools like Random Trees, CHAID, K-Nearest Neighbor, or Naïve Bayes [43]. Although they are not so new, Artificial Neural Networks (ANN) have been used for years as a way to develop models based on data classification [35,42]. The combination of AI technologies and UAV imagery provides a robust modern base for developing new cost-effective empirical models, but there is still much research needed to improve their accuracy [44].

2.2. Dynamic Models

Dynamic models are based on mathematical approximations of natural processes, based on equations that have no linear behavior and have an important number of variables. There are many processes that have been incorporated into the dynamic models; the most common are the carbon cycle, nitrogen cycle, water dynamics, plant growth, and plant competition [25].
Using a dynamic model must be performed carefully; all the variables must be used according to model requirements, and in some cases, their objective determination is not easy and requires indirect determination from other parameters. This does not only increase correlation between variables; it is also a common source of error [21]. Most dynamic models are built on modules that simulate a specific cycle or process. Although those modules are often independent, their results will have an impact on the rest; the impact is usually not linear, so small changes in one module can lead to great differences in the result as a result of losing precision [45]. To be widely used, the model must be easy to use, have as few variables as possible, and be parametrized for as many conditions as possible. But finding a balance between user friendliness and accuracy is a complex challenge. As a result, precision increases its usability, and as a consequence, the number of users decreases [46,47,48].
In the case of meadows, the number of variables increases compared to other crops. Each species has a different lifespan; some plants are annual and others are pluriannual; their phenology varies between species; surviving rates will change depending on management, climate, and species. All this complexity leads to more challenging model-building [10,28]. To solve this problem, some models have simplified this process, and in some cases, they have obviated it, but at the cost of reducing model precision [49,50]. Simplification can be performed by aggregating growing patterns of vegetation and considering it as a single crop, making modeling easier [49].
One of the first models developed for meadows was the Hurley Pasture Model. It is a generic, deterministic, dynamic, and mechanistic model where the cycles of carbon, nitrogen, and water are simulated using modules to independently simulate each cycle in the soil, plant, and animal and apply its result to the rest of the modules. This model uses parameters like Leaf Area Index (LAI), Net Primary Productivity (NPP), root-shoot partitioning, C/N ratio, soil organic matter, etc. Some dynamical models have integrated this model into them as the backbone of meadow simulation [51].
There are many different dynamic models, but we can classify them according to their characteristics [25], as follows:
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Ecological model: they are small models focusing on biotic interactions using elegant equations. Those models explain general ecological patterns, including species interactions, but abiotic effects and spatial heterogeneity are poorly accounted for.
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Biogeochemical: they are parameter-rich models of the cycling of carbon, nutrients, and water. They make long-term predictions about biogeochemical cycles and soil pools. On the other hand, they usually have limited capacity for yield forecasting and limited capacity for heterogeneity and biodiversity.
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Agricultural: they are rich-parameter models focusing on phenology and yield formation. They make short-term predictions of productivity, but they lack long-term predictive capacity and admit no spatial heterogeneity or biodiversity.
In this paper, we have revised some of the dynamic models that have been used for meadow production. The selection criterion was the existence of bibliographical references regarding the application of the model for grassland management. Most of them are agricultural models due to their inherent focus on production. Ecological models, as they are not well suited for production, have not been considered. Some biochemical models, although they are not focused on production, can accurately predict production. All of them have global scope. Although some models are not calibrated for meadow production, there are popular agricultural models that have great potential in meadow modeling, and there are some studies where they have calibrated them for meadows in certain environments. There could be more models, such as GrassProg or CosMo, but putting more models into the review could be redundant, as some of the nonstudied models have a similar structure as the chosen ones. Table 1 shows some characteristics of these models and their main bibliographical references.
Table 2 provides additional information on the use of the models of management practices parameters (mowing, grazing, and fertilization), biodiversity parameters, and the volume of data needed to run them.

2.2.1. APSIM

The Agricultural Production System Simulator (APSIM) was originally developed in Australia, but it now suits all global conditions. Its aim is to have an easy-to-use model able to predict harvest according to different situations and to give the manager a useful tool to help in decision making. It has been parametrized for multiple crops, including meadows [52,53]. It has a modular architecture where different components represent specific processes in the system, like soil, weather, crop, and nutrients, where each component interacts with another [54]. For modeling crop growth, it simulates key processes such as photosynthesis, respiration, transpiration, and phenology using factors such as climate factors (temperature and solar radiation) and soil factors (soil moisture and nutrient availability), whereas crop development stages are tracked based on thermal accumulation [55]. It also models nutrients and water dynamics using soil properties, management practices, and crop characteristics to model soil water movement, evaporation, nutrient cycling, and water and nutrient uptake by the crop [56,57].
One of the greatest strengths of this model is its capability to define a wide range of management practices, like sowing, irrigation, fertilization, mowing, or grazing. Each practice can be customized to the studied conditions [58]. It is also noticeable for its ability to infer the growth of each species, simulating the effects of competition and grazing [59,60].

2.2.2. STICS

Simulateur mulTIdisciplinaire pour les Cultures Standard STICS, a model developed by the French National Institute for Agronomic Research (INRA), consists of a yield-focused agricultural model [61,62]. It also has a modular design where each module represents different aspects of the crop system, namely, soil, climate, crop, and management. Those modules interact with each other to simulate crop growth and development [62,63]. Plant growth is based on temperature using degree-fays, but it also considers other factors such as solar radiation, water, and nutrient availability [64]. It incorporates management data such as irrigation and fertilization [65].
Although its focus is on yield forecasting, it can also predict quality [66]. Another strength is that it makes it easy to change management dates, such as the sowing date or the mowing date, to evaluate their impact [67].

2.2.3. LINGRA

This model is especially designed to simulate grassland growth under various conditions [68,69]. It is simpler than other models and calculates three types of production, namely, potential production, water-limited production, and nitrogen-limited production [70]. It requires less input than other models. For weather, it only needs solar radiation, minimum and maximum temperatures, vapor pressure, wind speed, and rainfall. For the soil analysis, it just needs soil depth, moisture content at field capacity, saturation, and wilting point. And finally, for management, it only needs to know when the harvest is performed and when and how much fertilization is applied [69,71].
Its stronger point is its simplicity; it can even be run on Excel 17.0 [72]. It has been used successfully to estimate forage production in the European Union and is the model that better represents physiological mechanisms that take part in defoliation and regrowth [73].
As a drawback, it lacks reproductive growth, herbage growth from nitrogen fertilizer, species proportion, and herbage quality. Some studies have improved those parameters [74].

2.2.4. CROPSYST

This agricultural model is a multiyear, multicrop model that simulates crop growth on a daily basis. It is one of the most used models due to its user-friendly environment and its wide range of parametrized crops and conditions [75,76]. It has various modules that simulate the soil water budget, soil and plant nitrogen budget, crop growth, dry matter production, yield formation, residue production and decomposition, and soil erosion [77]. It calculates crop growth based on the thermal accumulation needed to reach a specific phonologic phase, although it also takes into account the limitations of water, nitrogen, light, or temperature [78].
It has the strength of being able to accurately predict the consequences of extreme climate events on crop phenology and development [79]. It has been bundled with ClimGen, a generator of weather conditions for places where there is not much data available. And it can be improved by the use of GIS [80]. Although there are many parametrized crops, meadows are not one of them, but some studies have parameterized them for certain meadow situations [81].

2.2.5. WOFOST

It is the acronym for WOrld FOod STudies (WOFOST), a mechanistic and dynamic agricultural model. It was developed by the Center for World Food Studies in collaboration with Wageningen University and Research [82,83]. It simulates crop growth on a daily basis, modeling natural processes like photosynthesis and respiration. It also considers limitations caused by temperature, light, water, and soil properties [84]. When the crop is parametrized, it requires little input about climate, management, and soil, making it easy to use [85]. As outputs, it gives the maximum yield achievable under optimal conditions, biomass accumulation, water use efficiency, and actual production [86].
This model is used worldwide to estimate crop yields around the globe, and their output is given by maps of yields. Despite being designed for crop yield estimation, it shows more accuracy in predicting crop growth and development than yield. In addition, remote sensing has been shown as a possible tool to improve its accuracy [85]. Unfortunately, it is not officially parametrized for grassland; some studies have achieved it [87,88].

2.2.6. PaSIM

It is the acronym for Pasture Simulation Model. It is a biochemical model designed to simulate grassland ecosystems by the INRA [89]. It is focused on carbon, nitrogen, and water flux throughout the soil–plant–atmosphere system. It accounts for net primary productivity, forage intake by domestic herbivores, and energy dynamics [90,91]. It requires a huge number of variables, accounting for more than 100, but only 27 have a significant impact [91]. As a difference from other models, it uses an hourly time step, allowing more detailed dynamics [92,93].
It is one of the most complete models, having a complete simulation of all the processes that affect meadows [94], even tackling the impact of grazing on production, but due to its complexity, it requires a fairly large amount of calibration study [95].

2.2.7. Biome-BCG

This model, originally developed by the University of Montana to simulate forest conditions, is a combination of a biogeochemical and an ecological model. It is capable of modeling interactions between nutrients and water cycles with species mortality and expansion [96,97]. It operates at a daily time step and requires a vast number of parameters, aggregated in four files, namely, one for initial conditions, a second for meteorological data, a third for eco-physiological constants, and the last with soil properties [98]. It is able to incorporate management information such as fertilization and grazing using a management file [99,100]. As an additional parameter, we can use NDVI, improving its accuracy [101].
It has the strength of being able to simulate all processes involved in meadows, giving precise information about not only yield but also carbon and nitrogen fluxes in the soil [97]. As a setback, it requires a lot of data to be calibrated because each meadow community will have a different behavior [102].

2.2.8. CenW

Acronym for Carbon Energy Nutrients Water is a biogeochemical model designed to study environmental responses to changes in the ecosystem [103]. It is mainly focused on physiology. It simulates the simplification of physiological plant processes such as photosynthesis and the cycles of nutrients and water. It requires fewer variables than other biogeochemical models. [104,105]. It has been mainly applied to study carbon balance in forests, but then it was adapted to grasslands [106,107].
It is the simpler of the biochemical models, but it is still capable of considering practices like grazing and irrigation [108,109].

3. Discussion

As it has been shown, there are many different types of meadow modeling; each of them has its weaknesses and its strengths.
Empirical models arise as the best tool to analyze a concrete situation, and current developments in AI and remote sensing make them more versatile. They are also very useful for making predictions within their data range, but if we need to make projections outside of their data range, their results will be highly speculative. Making them less reliable to predict outcomes from extreme weather conditions that have not been observed or management practices that have not been applied.
APSIM appears as a powerful tool to assess meadow production accounting, grazing, and mowing without the need for an extra model customization study. It performs equally well in warm climates as in cold climates [52,55]. Also, its user-friendly interface makes it usable. But most of the study is performed in Lolium sp. and Trifolium sp. pastures, not on seminatural meadows.
STICS is considered the agricultural model that better simulates nitrogen and water dynamics, but it is not parametrized for meadows [65].
LINGRA can be easily used with Python, R, or even Excel, and it has a robust defoliation and regrowth model, but all of its parametrizations are based on the grass monoculture of Lolium sp. or Dactylis glomerata [68,71,73].
CROPSYST is one of the most user-friendly models. It is capable of properly simulating most of the factors that affect plant growth and development. Although meadows are not parametrized, in some studies, they have been simplified as a monoculture of the dominant species [80,81].
WOFOST is a global model that can be used anywhere, and its graphical outputs are one of the easiest ways of visualizing results. But its design forces it to simplify meadows into a single crop, losing its accuracy [83,84,88].
PaSIM is developed specifically for meadows, and there are many papers where production has been accurately predicted. As a tradeoff, it needs to parametrize many parameters, making it more difficult to use [89,91,92,94].
Biome-BCG is the model that best represents meadow biodiversity and considers more ecological factors. Although it was not its main goal, it can predict production as well as agricultural models. But its high complexity makes it easy to make mistakes [99,101,106].
CenW is good at predicting carbon and nitrogen balance, especially useful to evaluate the implications of climate change in meadows, but is less accurate for predicting production than other models [105,106,109].
Some papers have compared various models. WOFOST and CROPSYST were used with similar results [29]. APIM was compared with GrassProg1, a simpler model for grasses, with no significant difference [110]. Biome-GCG and PaSIM were compared, and the only significant difference was that PaSIM estimated better evapotranspiration [97].
It is possible to aggregate model results into an ensemble model, which combines the characteristics of both empirical and dynamic models [13]. They are the combination of results from different models, which gives them higher robustness [31,90,111]. This combination can be performed in various ways, such as by building it using the median of all simulations or by weighting according to each error [111]. Ensemble models have shown higher accuracy than other models, but it requires calibrating and parametrizing all the models that want to be combined. It is a highly labor-intensive method [90,111].
Most models simplify meadow biodiversity into one virtual crop, acting as if the meadow is a monolithic living structure that does not change with time. But their compositions vary depending mainly on climate and management [49]. Obviating those changes could lead to errors, due to the changes in vegetation that will result in response changes. Taking vegetation changes into the model does not come for free; it increases its complexity and makes it more complex to use [13]. Some factors are not considered by any model. For instance, meadow floristic composition will affect nitrogen content in animal depositions, and all models consider it stable [112,113]. Also, its distribution would not be uniform; animals tend to spend more time in some places than others, changing soil dynamics and biodiversity at a local level [114].
Any model considers soil erosion, which could be driven by overgrazing. Loss of soil would decrease meadow productivity in the long term [115]. Being a key component of livestock farming, the economic productivity of meadows must be considered, and only a few dynamic models, such as APSIM, take this into account [116]. Lastly, all models require precise climate data, usually temperature, rain, radiation, and wind. Given mountain orography, weather conditions can be abruptly different at low distances, adding to the need for more data acquisition [117]. As climate data are usually obtained from close locations, it can be inaccurate due to the orographic differences, which would lead to errors in the predictions.
New technologies open great opportunities to improve meadow modeling [118]. Using remote sensing makes it possible to get new objective variables at a relatively low work load cost, enhancing model robustness [119,120]. In addition, the use of animal monitoring sensors, can help obtain more data about animal behavior in the meadow, making animal grazing dynamics less speculative and more objective [121].
Climate change is one of the biggest challenges that meadows face. Due to its complexity, it is difficult to determine what practices are best suited to face it. Using models, we can anticipate its consequences and evaluate possible adaptation and mitigation practices. Although much has been studied, we still need to improve models and analyze them to find the best practices [116,122].

4. Conclusions

Mountain meadow production modeling is a difficult task. It is formed by many different species, and their management is complex, combining grazing and mowing. Empirical models can make good predictions inside their data range, but they can be very inaccurate outside. There are many dynamic models that can estimate production, but many of them are not parametrized for meadows or are data-intensive and complex to use.
Many models tend to focus on environmental parameters such as carbon or nitrogen fluxes or tend to simplify meadows into a virtual single crop. Despite the huge amount of information available for meadow modeling, there is little information about production modeling in meadows.
There is still study to do to tackle the challenge of vegetation changes and obtain better climate data for mountainous areas. Otherwise, we do not really know how mountain meadows will respond to the coming changes or which practices we should endorse to make them economic and environmentally sustainable.

Author Contributions

Conceptualization, A.J., A.U. and R.R.; methodology, A.J., A.U. and R.R.; investigation, A.U. and R.R.; resources, A.J.; data curation, A.J.; writing—original draft preparation, A.J.; writing—review and editing, A.J., A.U. and R.R.; supervision, A.U. and R.R.; project administration, R.R.; funding acquisition, R.R. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by the Gobierno de Aragón, Project number: GCP2021000100 (Programa de Desarrollo Rural para Aragón 2014–2020, Departamento de Desarrollo Rural y Sostenibilidad del Gobierno de Aragón), and the European Agricultural Fund for Rural Development, European Union.

Data Availability Statement

Data can be shared with other researchers upon request for collaboration.

Acknowledgments

The authors would like to thank Joaquín Ascaso for his work and dedication and for having the farmers collaborate on this project.

Conflicts of Interest

The authors declare no conflicts of interest.

References

  1. Janišová, M.; Bojko, I.; Ivașcu, C.M.; Iuga, A.; Biro, A.-S.; Magnes, M. Grazing Hay Meadows: History, Distribution, and Ecological Context. Appl. Veg. Sci. 2023, 26, e12723. [Google Scholar] [CrossRef]
  2. Ascaso, J.; Reiné, R.; Barrantes, O. Evolution of Hay Meadows between 1956, 1986, and 2016 and Its Relation to the Characteristics and Location of the Parcels in the Valley of the River Esera (Pyrenees, Spain). Agronomy 2020, 10, 329. [Google Scholar] [CrossRef]
  3. Hejcman, M.; Hejcmanová, P.; Pavlů, V.; Beneš, J. Origin and History of Grasslands in Central Europe—A Review. Grass Forage Sci. 2013, 68, 345–363. [Google Scholar] [CrossRef]
  4. Peeters, A. Environmental Impacts and Future Challenges of Grasslands and Grassland-Based Livestock Production Systems in Europe. In Grasslands: A Global Resource Perspective; Army Printing Press: Lucknow, India, 2015; pp. 365–390. [Google Scholar]
  5. Puche, N.; Senapati, N.; Flechard, C.R.; Klumpp, K.; Kirschbaum, M.U.F.; Chabbi, A. Modeling Carbon and Water Fluxes of Managed Grasslands: Comparing Flux Variability and Net Carbon Budgets between Grazed and Mowed Systems. Agronomy 2019, 9, 183. [Google Scholar] [CrossRef]
  6. Li, Z.; Huffman, T.; McConkey, B.; Townley-Smith, L. Monitoring and Modeling Spatial and Temporal Patterns of Grassland Dynamics Using Time-Series MODIS NDVI with Climate and Stocking Data. Remote Sens. Environ. 2013, 138, 232–244. [Google Scholar] [CrossRef]
  7. Wätzold, F.; Drechsler, M.; Johst, K.; Mewes, M.; Sturm, A. A Novel, Spatiotemporally Explicit Ecological-Economic Modeling Procedure for the Design of Cost-Effective Agri-Environment Schemes to Conserve Biodiversity. Am. J. Agric. Econ. 2016, 98, 489–512. [Google Scholar] [CrossRef]
  8. Klimek, S.; gen Kemmermann, A.R.; Hofmann, M.; Isselstein, J. Plant Species Richness and Composition in Managed Grasslands: The Relative Importance of Field Management and Environmental Factors. Biol. Conserv. 2007, 134, 559–570. [Google Scholar] [CrossRef]
  9. Jones, J.A.; Hutchinson, R.; Moldenke, A.; Pfeiffer, V.; Helderop, E.; Thomas, E.; Griffin, J.; Reinholtz, A. Landscape Patterns and Diversity of Meadow Plants and Flower-Visitors in a Mountain Landscape. Landsc. Ecol. 2019, 34, 997–1014. [Google Scholar] [CrossRef]
  10. Siehoff, S.; Lennartz, G.; Heilburg, I.C.; Roß-Nickoll, M.; Ratte, H.T.; Preuss, T.G. Process-Based Modeling of Grassland Dynamics Built on Ecological Indicator Values for Land Use. Ecol. Model. 2011, 222, 3854–3868. [Google Scholar] [CrossRef]
  11. Barrachina, M.; Cristóbal, J.; Tulla, A.F. Estimating Above-Ground Biomass on Mountain Meadows and Pastures through Remote Sensing. Int. J. Appl. Earth Obs. Geoinf. 2015, 38, 184–192. [Google Scholar] [CrossRef]
  12. Dengler, J.; Janišová, M.; Török, P.; Wellstein, C. Biodiversity of Palaearctic Grasslands: A Synthesis. Agric. Ecosyst. Environ. 2014, 182, 1–14. [Google Scholar] [CrossRef]
  13. Van Oijen, M.; Barcza, Z.; Confalonieri, R.; Korhonen, P.; Kröel-Dulay, G.; Lellei-Kovács, E.; Louarn, G.; Louault, F.; Martin, R.; Moulin, T.; et al. Incorporating Biodiversity into Biogeochemistry Models to Improve Prediction of Ecosystem Services in Temperate Grasslands: Review and Roadmap. Agronomy 2020, 10, 259. [Google Scholar] [CrossRef]
  14. Socher, S.A.; Prati, D.; Boch, S.; Müller, J.; Baumbach, H.; Gockel, S.; Hemp, A.; Schöning, I.; Wells, K.; Buscot, F.; et al. Interacting Effects of Fertilization, Mowing and Grazing on Plant Species Diversity of 1500 Grasslands in Germany Differ between Regions. Basic Appl. Ecol. 2013, 14, 126–136. [Google Scholar] [CrossRef]
  15. Blüthgen, N.; Dormann, C.F.; Prati, D.; Klaus, V.H.; Kleinebecker, T.; Hölzel, N.; Alt, F.; Boch, S.; Gockel, S.; Hemp, A.; et al. A Quantitative Index of Land-Use Intensity in Grasslands: Integrating Mowing, Grazing and Fertilization. Basic Appl. Ecol. 2012, 13, 207–220. [Google Scholar] [CrossRef]
  16. Murphy, D.J.; Shine, P.; Brien, B.O.; Donovan, M.O.; Murphy, M.D. Utilising Grassland Management and Climate Data for More Accurate Prediction of Herbage Mass Using the Rising Plate Meter. Precis. Agric. 2021, 22, 1189–1216. [Google Scholar] [CrossRef]
  17. Woodward, S.; Rollo, M. Why Pasture Growth Prediction Is Difficult. Agron. Soc. N. Z. 2002, 32, 17–26. [Google Scholar]
  18. Socher, S.A.; Prati, D.; Boch, S.; Müller, J.; Klaus, V.H.; Hölzel, N.; Fischer, M. Direct and Productivity-Mediated Indirect Effects of Fertilization, Mowing and Grazing on Grassland Species Richness. J. Ecol. 2012, 100, 1391–1399. [Google Scholar] [CrossRef]
  19. Fischer, T.; Byerlee, D.; Edmeades, G. Crop Yields and Global Food Security: Will Yield Increase Continue to Feed the World? Australian Centre for International Agricultural Research: Canberra, ACT, Australia, 2014. [Google Scholar]
  20. Aggarwal, P.K.; Kalra, N. Analyzing the Limitations Set by Climatic Factors, Genotype, and Water and Nitrogen Availability on Productivity of Wheat II. Climatically Potential Yields and Management Strategies. Field Crops Res. 1994, 38, 93–103. [Google Scholar] [CrossRef]
  21. Bellocchi, G.; Rivington, M.; Donatelli, M.; Matthews, K. Validation of Biophysical Models: Issues and Methodologies. A Review. Agron. Sustain. Dev. 2010, 30, 109–130. [Google Scholar] [CrossRef]
  22. Malik, W.; Boote, K.J.; Hoogenboom, G.; Cavero, J.; Dechmi, F. Adapting the CROPGRO Model to Simulate Alfalfa Growth and Yield. Agron. J. 2018, 110, 1777–1790. [Google Scholar] [CrossRef]
  23. Neupane, D.; Adhikari, P.; Bhattarai, D.; Rana, B.; Ahmed, Z.; Sharma, U.; Adhikari, D. Does Climate Change Affect the Yield of the Top Three Cereals and Food Security in the World? Earth 2022, 3, 45–71. [Google Scholar] [CrossRef]
  24. Webber, H.; Gaiser, T.; Ewert, F. What Role Can Crop Models Play in Supporting Climate Change Adaptation Decisions to Enhance Food Security in Sub-Saharan Africa? Agric. Syst. 2014, 127, 161–177. [Google Scholar] [CrossRef]
  25. Van Oijen, M.; Bellocchi, G.; Höglind, M. Effects of Climate Change on Grassland Biodiversity and Productivity: The Need for a Diversity of Models. Agronomy 2018, 8, 14. [Google Scholar] [CrossRef]
  26. Zhao, Y.; Wang, X.; Chen, F.; Li, J.; Wu, J.; Sun, Y.; Zhang, Y.; Deng, T.; Jiang, S.; Zhou, X.; et al. Soil Organic Matter Enhances Aboveground Biomass in Alpine Grassland under Drought. Geoderma 2023, 433, 116430. [Google Scholar] [CrossRef]
  27. Fer, I.; Kelly, R.; Moorcroft, P.R.; Richardson, A.D.; Cowdery, E.M.; Dietze, M.C. Linking Big Models to Big Data: Efficient Ecosystem Model Calibration through Bayesian Model Emulation. Biogeosciences 2018, 15, 5801–5830. [Google Scholar] [CrossRef]
  28. Höglind, M.; Cameron, D.; Persson, T.; Huang, X.; van Oijen, M. BASGRA_N: A Model for Grassland Productivity, Quality and Greenhouse Gas Balance. Ecol. Model. 2020, 417, 108925. [Google Scholar] [CrossRef]
  29. Movedi, E.; Bellocchi, G.; Argenti, G.; Paleari, L.; Vesely, F.; Staglianò, N.; Dibari, C.; Confalonieri, R. Development of Generic Crop Models for Simulation of Multi-Species Plant Communities in Mown Grasslands. Ecol. Model. 2019, 401, 111–128. [Google Scholar] [CrossRef]
  30. Meng, B.; Ge, J.; Liang, T.; Yang, S.; Gao, J.; Feng, Q.; Cui, X.; Huang, X.; Xie, H. Evaluation of Remote Sensing Inversion Error for the Above-Ground Biomass of Alpine Meadow Grassland Based on Multi-Source Satellite Data. Remote Sens. 2017, 9, 372. [Google Scholar] [CrossRef]
  31. Wu, D.; Ciais, P.; Viovy, N.; Knapp, A.K.; Wilcox, K.; Bahn, M.; Smith, M.D.; Vicca, S.; Fatichi, S.; Zscheischler, J.; et al. Asymmetric Responses of Primary Productivity to Altered Precipitation Simulated by Ecosystem Models across Three Long-Term Grassland Sites. Biogeosciences 2018, 15, 3421–3437. [Google Scholar] [CrossRef]
  32. Sándor, R.; Ehrhardt, F.; Grace, P.; Recous, S.; Smith, P.; Snow, V.; Soussana, J.-F.; Basso, B.; Bhatia, A.; Brilli, L.; et al. Residual Correlation and Ensemble Modelling to Improve Crop and Grassland Models. Environ. Model. Softw. 2023, 161, 105625. [Google Scholar] [CrossRef]
  33. Shaffer, J.A.; Roth, C.L.; Mushet, D.M. Modeling Effects of Crop Production, Energy Development and Conservation-Grassland Loss on Avian Habitat. PLoS ONE 2019, 14, e0198382. [Google Scholar] [CrossRef]
  34. Tredennick, A.T.; Hooker, G.; Ellner, S.P.; Adler, P.B. A Practical Guide to Selecting Models for Exploration, Inference, and Prediction in Ecology. Ecology 2021, 102, e03336. [Google Scholar] [CrossRef] [PubMed]
  35. Tan, S.S.; Smeins, F.E. Predicting Grassland Community Changes with an Artificial Neural Network Model. Ecol. Model. 1996, 84, 91–97. [Google Scholar] [CrossRef]
  36. Liu, H.; Gong, Y.; Li, Y.; Liu, S.; Yu, Z.; Zhao, R. Does Grazing Exclusion Enhance Grassland Restoration? Evidence from Northern China. Ecol. Indic. 2023, 149, 110166. [Google Scholar] [CrossRef]
  37. Baghdadi, N.; El Hajj, M.; Zribi, M.; Bousbih, S. Calibration of the Water Cloud Model at C-Band for Winter Crop Fields and Grasslands. Remote Sens. 2017, 9, 969. [Google Scholar] [CrossRef]
  38. Gu, Y.; Boyte, S.P.; Wylie, B.K.; Tieszen, L.L. Identifying Grasslands Suitable for Cellulosic Feedstock Crops in the Greater Platte River Basin: Dynamic Modeling of Ecosystem Performance with 250 m eMODIS. GCB Bioenergy 2012, 4, 96–106. [Google Scholar] [CrossRef]
  39. Courault, D.; Hadria, R.; Ruget, F.; Olioso, A.; Duchemin, B.; Hagolle, O.; Dedieu, G. Combined Use of FORMOSAT-2 Images with a Crop Model for Biomass and Water Monitoring of Permanent Grassland in Mediterranean Region. Hydrol. Earth Syst. Sci. 2010, 14, 1731–1744. [Google Scholar] [CrossRef]
  40. Possoch, M.; Bieker, S.; Hoffmeister, D.; Bolten, A.; Schellberg, J.; Bareth, G. Multi-Temporal Crop Surface Models Combined with the RGB Vegetation Index from UAV-Based Image for Forage Monitoring in Grassland. ISPRS—Int. Arch. Photogramm. Remote Sens. Spat. Inf. Sci. 2016, XLI-B1, 991–998. [Google Scholar] [CrossRef]
  41. Wijesingha, J.; Moeckel, T.; Hensgen, F.; Wachendorf, M. Evaluation of 3D Point Cloud-Based Models for the Prediction of Grassland Biomass. Int. J. Appl. Earth Obs. Geoinf. 2019, 78, 352–359. [Google Scholar] [CrossRef]
  42. Yang, S.; Feng, Q.; Liang, T.; Liu, B.; Zhang, W.; Xie, H. Modeling Grassland Above-Ground Biomass Based on Artificial Neural Network and Remote Sensing in the Three-River Headwaters Region. Remote Sens. Environ. 2018, 204, 448–455. [Google Scholar] [CrossRef]
  43. Pudumalar, S.; Ramanujam, E.; Rajashree, R.H.; Kavya, C.; Kiruthika, T.; Nisha, J. Crop Recommendation System for Precision Agriculture. In Proceedings of the 2016 Eighth International Conference on Advanced Computing (ICoAC), Chennai, India, 19–21 January 2017; pp. 32–36. [Google Scholar]
  44. De Rosa, D.; Basso, B.; Fasiolo, M.; Friedl, J.; Fulkerson, B.; Grace, P.R.; Rowlings, D.W. Predicting Pasture Biomass Using a Statistical Model and Machine Learning Algorithm Implemented with Remotely Sensed Imagery. Comput. Electron. Agric. 2021, 180, 105880. [Google Scholar] [CrossRef]
  45. Cavalli, D.; Bellocchi, G.; Corti, M.; Marino Gallina, P.; Bechini, L. Sensitivity Analysis of C and N Modules in Biogeochemical Crop and Grassland Models Following Manure Addition to Soil. Eur. J. Soil Sci. 2019, 70, 833–846. [Google Scholar] [CrossRef]
  46. Andales, A.A.; Derner, J.D.; Ahuja, L.R.; Hart, R.H. Strategic and Tactical Prediction of Forage Production in Northern Mixed-Grass Prairie. Rangel. Ecol. Manag. 2006, 59, 576–584. [Google Scholar] [CrossRef]
  47. Corson, M.S.; Rotz, C.A.; Skinner, R.H. Evaluating Warm-Season Grass Production in Temperate-Region Pastures: A Simulation Approach. Agric. Syst. 2007, 93, 252–268. [Google Scholar] [CrossRef]
  48. Hanrahan, L.; Geoghegan, A.; O’Donovan, M.; Griffith, V.; Ruelle, E.; Wallace, M.; Shalloo, L. PastureBase Ireland: A Grassland Decision Support System and National Database. Comput. Electron. Agric. 2017, 136, 193–201. [Google Scholar] [CrossRef]
  49. Fu, L.; Bo, T.; Du, G.; Zheng, X. Modeling the Responses of Grassland Vegetation Coverage to Grazing Disturbance in an Alpine Meadow. Ecol. Model. 2012, 247, 221–232. [Google Scholar] [CrossRef]
  50. Wang, H.; Ma, M.; Wang, X.; Yuan, W.; Song, Y.; Tan, J.; Huang, G. Seasonal Variation of Vegetation Productivity over an Alpine Meadow in the Qinghai–Tibet Plateau in China: Modeling the Interactions of Vegetation Productivity, Phenology, and the Soil Freeze–Thaw Process. Ecol. Res. 2013, 28, 271–282. [Google Scholar] [CrossRef]
  51. Thornley, J.H.M.; Cannell, M.G.R. Temperate Grassland Responses to Climate Change: An Analysis Using the Hurley Pasture Model. Ann. Bot. 1997, 80, 205–221. [Google Scholar] [CrossRef]
  52. Korhonen, P.; Palosuo, T.; Persson, T.; Höglind, M.; Jégo, G.; Van Oijen, M.; Gustavsson, A.-M.; Bélanger, G.; Virkajärvi, P. Modelling Grass Yields in Northern Climates—A Comparison of Three Growth Models for Timothy. Field Crops Res. 2018, 224, 37–47. [Google Scholar] [CrossRef]
  53. Pembleton, K.G.; Rawnsley, R.P.; Jacobs, J.L.; Mickan, F.J.; O’Brien, G.N.; Cullen, B.R.; Ramilan, T. Evaluating the Accuracy of the Agricultural Production Systems Simulator (APSIM) Simulating Growth, Development, and Herbage Nutritive Characteristics of Forage Crops Grown in the South-Eastern Dairy Regions of Australia. Crop Pasture Sci. 2013, 64, 147–164. [Google Scholar] [CrossRef]
  54. Holzworth, D.P.; Huth, N.I.; deVoil, P.G.; Zurcher, E.J.; Herrmann, N.I.; McLean, G.; Chenu, K.; van Oosterom, E.J.; Snow, V.; Murphy, C.; et al. APSIM—Evolution towards a New Generation of Agricultural Systems Simulation. Environ. Model. Softw. 2014, 62, 327–350. [Google Scholar] [CrossRef]
  55. Cichota, R.; Snow, V. Simulating Diverse Pastures with APSIM. Agron. Soc. N. Z. 2018, 48, 77–89. [Google Scholar]
  56. Moot, D.; Hargreaves, J.; Brown, H.; Teixeira, E. Calibration of the APSIM-Lucerne Model for ‘Grasslands Kaituna’ Lucerne Crops Grown in New Zealand. N. Z. J. Agric. Res. 2015, 58, 190–202. [Google Scholar] [CrossRef]
  57. Hoffmann, M.P.; Isselstein, J.; Rötter, R.P.; Kayser, M. Nitrogen Management in Crop Rotations after the Break-up of Grassland: Insights from Modelling. Agric. Ecosyst. Environ. 2018, 259, 28–44. [Google Scholar] [CrossRef]
  58. Robertson, M.; Carberry, P.; Huth, N.; Turpin, J.; Probert, M.; Poulton, P.; Bell, M.; Wright, G.; Yeates, S.; Brinsmead, R. Simulation of Growth and Development of Diverse Legume Species in APSIM. Crop Pasture Sci. 2002, 53, 429–446. [Google Scholar] [CrossRef]
  59. Li, F.Y.; Snow, V.; Johnson, I. Integration of a Pasture Model into APSIM. In Proceedings of the 15th Agronomy Conference 2010, Lincoln, New Zealand, 15–19 November 2010. [Google Scholar]
  60. Craig, P.R.; Badgery, W.; Millar, G.; Moore, A. Achieving Modelling of Pasture-Cropping Systems with APSIM and GRAZPLAN. In Proceedings of the 17th Australian Agronomy Conference 2015, Hobart, TAS, Australia, 20–24 September 2015. [Google Scholar]
  61. Brisson, N.; Gary, C.; Justes, E.; Roche, R.; Mary, B.; Ripoche, D.; Zimmer, D.; Sierra, J.; Bertuzzi, P.; Burger, P.; et al. An Overview of the Crop Model Stics. Eur. J. Agron. 2003, 18, 309–332. [Google Scholar] [CrossRef]
  62. Beaudoin, N.; Lecharpentier, P.; Ripoche-Wachter, D.; Strullu, L.; Mary, B.; Léonard, J.; Launay, M.; Justes, E. (Eds.) STICS Soil-Crop Model: Conceptual Framework, Equations and Uses; Éditions Quae: Versailles, France, 2023. [Google Scholar]
  63. Brilli, L.; Bechini, L.; Bindi, M.; Carozzi, M.; Cavalli, D.; Conant, R.; Dorich, C.D.; Doro, L.; Ehrhardt, F.; Farina, R.; et al. Review and Analysis of Strengths and Weaknesses of Agro-Ecosystem Models for Simulating C and N Fluxes. Sci. Total Environ. 2017, 598, 445–470. [Google Scholar] [CrossRef] [PubMed]
  64. Kherif, O.; Seghouani, M.; Justes, E.; Plaza-Bonilla, D.; Bouhenache, A.; Zemmouri, B.; Dokukin, P.; Latati, M. The First Calibration and Evaluation of the STICS Soil-Crop Model on Chickpea-Based Intercropping System under Mediterranean Conditions. Eur. J. Agron. 2022, 133, 126449. [Google Scholar] [CrossRef]
  65. Jing, Q.; Jégo, G.; Bélanger, G.; Chantigny, M.H.; Rochette, P. Simulation of Water and Nitrogen Balances in a Perennial Forage System Using the STICS Model. Field Crops Res. 2017, 201, 10–18. [Google Scholar] [CrossRef]
  66. Meyer, N.; Bergez, J.-E.; Justes, E.; Constantin, J. Influence of Cover Crop on Water and Nitrogen Balances and Cash Crop Yield in a Temperate Climate: A Modelling Approach Using the STICS Soil-Crop Model. Eur. J. Agron. 2022, 132, 126416. [Google Scholar] [CrossRef]
  67. Yin, X.; Beaudoin, N.; Ferchaud, F.; Mary, B.; Strullu, L.; Chlébowski, F.; Clivot, H.; Herre, C.; Duval, J.; Louarn, G. Long-Term Modelling of Soil N Mineralization and N Fate Using STICS in a 34-Year Crop Rotation Experiment. Geoderma 2020, 357, 113956. [Google Scholar] [CrossRef]
  68. Schapendonk, A.H.C.M.; Stol, W.; van Kraalingen, D.W.G.; Bouman, B.A.M. LINGRA, a Sink/Source Model to Simulate Grassland Productivity in Europe. Eur. J. Agron. 1998, 9, 87–100. [Google Scholar] [CrossRef]
  69. Giannitsopoulos, M.; Burgess, P.; Richter, G.M.; Bell, M.; Topp, C.F.E.; Ingram, J.; Takahashi, T. LINGRA-N Grassland Management Tool. Available online: https://cord.cranfield.ac.uk/ndownloader/articles/11359613/versions/5 (accessed on 15 March 2024).
  70. Pogačar, T.; Ipavec, D.; Verbič, J.; Kajfež-Bogataj, L. Calibration of the LINGRA-N Model to Simulate Herbage Yield of Grass Monocultures and Permanent Grassland in Slovenia. Acta Agric. Slov. 2015, 105, 111–123. [Google Scholar] [CrossRef]
  71. Pogačar, T.; Bogataj, L.K. Simulation of Grass Sward Dry Matter Yield in Slovenia Using the LINGRA-N Model. Ital. J. Agron. 2018, 13, 44–56. [Google Scholar] [CrossRef]
  72. Giannitsopoulos, M.L.; Burgess, P.J.; Richter, G.M.; Bell, M.J.; Topp, C.F.E.; Ingram, J.; Takahashi, T. Modelling the Interactions of Soils, Climate, and Management for Grass Production in England and Wales. Agronomy 2021, 11, 677. [Google Scholar] [CrossRef]
  73. Stol, W.; Bouman, B.A.M.; Schapendonk, H.C.M. Timely and Regional Monitoring of Forage Production in the European Union: The LINGRA Model. In Proceedings of the Second SAI Annual Users’ Seminars, Baveno Italy, 21–22 May 1998. [Google Scholar]
  74. Barrett, P.D.; Laidlaw, A.S.; Mayne, C.S. Development of a European Herbage Growth Model (the EU Grazemore Project). Land use systems in grassland dominated regions. In Proceedings of the 20th General Meeting of the European Grassland Federation, Luzern, Switzerland, 21–24 June 2004. [Google Scholar]
  75. Suárez-Rey, E.M.; Romero-Gámez, M.; Giménez, C.; Thompson, R.B.; Gallardo, M. Use of EU-Rotate_N and CropSyst Models to Predict Yield, Growth and Water and N Dynamics of Fertigated Leafy Vegetables in a Mediterranean Climate and to Determine N Fertilizer Requirements. Agric. Syst. 2016, 149, 150–164. [Google Scholar] [CrossRef]
  76. Stockle, C.O.; Cabelguenne, M.; Debaeke, P. Comparison of CropSyst Performance for Water Management in Southwestern France Using Submodels of Different Levels of Complexity. Eur. J. Agron. 1997, 7, 89–98. [Google Scholar] [CrossRef]
  77. Stockle, C.O.; Martin, S.A.; Campbell, G.S. CropSyst, a Cropping Systems Simulation Model: Water/Nitrogen Budgets and Crop Yield. Agric. Syst. 1994, 46, 335–359. [Google Scholar] [CrossRef]
  78. Piseddu, F. Knowledge Synthesis and Process-Based Modelling of Relationships between Plant Diversity, Environment and Management in Grasslands. Ph.D. Thesis, Université Clermont Auvergne, Clermont-Ferrand, France, 2022. [Google Scholar]
  79. Saseendran, S.A.; Ahuja, L.R.; Ma, L.; Timlin, D.; Stöckle, C.O.; Boote, K.J.; Hoogenboom, G. Current Water Deficit Stress Simulations in Selected Agricultural System Models. In Response of Crops to Limited Water; John Wiley & Sons, Ltd.: Hoboken, NJ, USA, 2008; pp. 1–38. ISBN 978-0-89118-188-0. [Google Scholar]
  80. Morari, F.; Lugato, E.; Borin, M. An Integrated Non-Point Source Model-GIS System for Selecting Criteria of Best Management Practices in the Po Valley, North Italy. Agric. Ecosyst. Environ. 2004, 102, 247–262. [Google Scholar] [CrossRef]
  81. Pravia, M.V.; Kemanian, A.R.; Terra, J.A. Soil Carbon and Nitrogen Dynamics of Integrated Crop-Pasture Systems with Annual and Perennial Forages. In Proceedings of the XXII International Grassland Congress, Sydney, Australia, 15–19 September 2013. [Google Scholar]
  82. de Wit, A.; Boogaard, H.; Fumagalli, D.; Janssen, S.; Knapen, R.; van Kraalingen, D.; Supit, I.; van der Wijngaart, R.; van Diepen, K. 25 Years of the WOFOST Cropping Systems Model. Agric. Syst. 2019, 168, 154–167. [Google Scholar] [CrossRef]
  83. Wang, X.; Johnson, D.L. Parameterization of WOFOST for a Typical Eurasian Steppe Grassland. In Proceedings of the Fall Meeting 2018, Washington, DC, USA, 10–14 December 2018. [Google Scholar]
  84. Kroes, J.G.; Supit, I. Impact Analysis of Drought, Water Excess and Salinity on Grass Production in The Netherlands Using Historical and Future Climate Data. Agric. Ecosyst. Environ. 2011, 144, 370–381. [Google Scholar] [CrossRef]
  85. Zhang, X.; He, B.; Quan, X. Assimilation of 30m Resolution LAI into Crop Growth Model for Improving LAI Estimation in Plateau Grassland. In Proceedings of the 2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS), Beijing, China, 10–15 July 2016; pp. 1296–1299. [Google Scholar]
  86. Camargo, G.G.T.; Kemanian, A.R. Six Crop Models Differ in Their Simulation of Water Uptake. Agric. For. Meteorol. 2016, 220, 116–129. [Google Scholar] [CrossRef]
  87. Zhang, Y.; Shu, Q.; Wang, L.; Quan, X.; Liu, X.; Lu, B. Estimation of Fuel Biomass for Grasslands Using Data Assimilation Technique. In Proceedings of the IGARSS 2019—2019 IEEE International Geoscience and Remote Sensing Symposium, Yokohama, Japan, 28 July–2 August 2019; pp. 9988–9991. [Google Scholar]
  88. Piseddu, F.; Hadj Saadi, D.; Movedi, M.; Picon-Cochard, C.; Roggero, P.P.; Confalonieri, R.; Bellocchi, G.; Seddaiu, G. Modelling Multi-Species Grasslands with Plant-Specific Suitability Functions. In Proceedings of the 28th EGF General Meeting on “Meeting the Future Demands for Grassland Production” Grassland Science in Europe, Online, 19–21 October 2020; Volume 25, p. 541. [Google Scholar]
  89. Pulina, A.; Lai, R.; Salis, L.; Seddaiu, G.; Roggero, P.P.; Bellocchi, G. Modelling Pasture Production and Soil Temperature, Water and Carbon Fluxes in Mediterranean Grassland Systems with the Pasture Simulation Model. Grass Forage Sci. 2018, 73, 272–283. [Google Scholar] [CrossRef]
  90. Graux, A.-I.; Bellocchi, G.; Lardy, R.; Soussana, J.-F. Ensemble Modelling of Climate Change Risks and Opportunities for Managed Grasslands in France. Agric. For. Meteorol. 2013, 170, 114–131. [Google Scholar] [CrossRef]
  91. Ben Touhami, H.; Lardy, R.; Barra, V.; Bellocchi, G. Screening Parameters in the Pasture Simulation Model Using the Morris Method. Ecol. Model. 2013, 266, 42–57. [Google Scholar] [CrossRef]
  92. Graux, A.-I.; Gaurut, M.; Agabriel, J.; Baumont, R.; Delagarde, R.; Delaby, L.; Soussana, J.-F. Development of the Pasture Simulation Model for Assessing Livestock Production under Climate Change. Agric. Ecosyst. Environ. 2011, 144, 69–91. [Google Scholar] [CrossRef]
  93. Ben Touhami, H.; Bellocchi, G. Bayesian Calibration of the Pasture Simulation Model (PaSim) to Simulate European Grasslands under Water Stress. Ecol. Inform. 2015, 30, 356–364. [Google Scholar] [CrossRef]
  94. Aghajanzadeh-Darzi, P.; Martin, R.; Laperche, S.; Jayet, P.-A. Climate Change Impacts on European Agriculture Revisited: Adding the Economic Dimension of Grasslands. Reg. Environ. Chang. 2017, 17, 261–272. [Google Scholar] [CrossRef]
  95. Riedo, M.; Gyalistras, D.; Fuhrer, J. Net Primary Production and Carbon Stocks in Differently Managed Grasslands: Simulation of Site-Specific Sensitivity to an Increase in Atmospheric CO2 and to Climate Change. Ecol. Model. 2000, 134, 207–227. [Google Scholar] [CrossRef]
  96. Sun, Q.; Li, B.; Zhang, T.; Yuan, Y.; Gao, X.; Ge, J.; Li, F.; Zhang, Z. An Improved Biome-BGC Model for Estimating Net Primary Productivity of Alpine Meadow on the Qinghai-Tibet Plateau. Ecol. Model. 2017, 350, 55–68. [Google Scholar] [CrossRef]
  97. Sándor, R.; Barcza, Z.; Hidy, D.; Lellei-Kovács, E.; Ma, S.; Bellocchi, G. Modelling of Grassland Fluxes in Europe: Evaluation of Two Biogeochemical Models. Agric. Ecosyst. Environ. 2016, 215, 1–19. [Google Scholar] [CrossRef]
  98. Sanchez-Ruiz, S.; Chiesi, M.; Fibbi, L.; Carrara, A.; Maselli, F.; Gilabert, M.A. Optimized Application of Biome-BGC for Modeling the Daily GPP of Natural Vegetation over Peninsular Spain. J. Geophys. Res. Biogeosci. 2018, 123, 531–546. [Google Scholar] [CrossRef]
  99. Hidy, D.; Barcza, Z.; Haszpra, L.; Churkina, G.; Pintér, K.; Nagy, Z. Development of the Biome-BGC Model for Simulation of Managed Herbaceous Ecosystems. Ecol. Model. 2012, 226, 99–119. [Google Scholar] [CrossRef]
  100. Tomelleri, E. Modeling the Carbon Cycle and Its Interactions with Management Practices in Grasslands; Study University of Padova: Padua, Italy, 2007. [Google Scholar]
  101. Maselli, F.; Argenti, G.; Chiesi, M.; Angeli, L.; Papale, D. Simulation of Grassland Productivity by the Combination of Ground and Satellite Data. Agric. Ecosyst. Environ. 2013, 165, 163–172. [Google Scholar] [CrossRef]
  102. Lellei-Kovács, E.; Barcza, Z.; Hidy, D.; Horváth, F.; Ittzés, D.; Ittzés, P.; Ma, S.; Bellocchi, G. Application of Biome-BGC MuSo in Managed Grassland Ecosystems in the Euro-Mediteranean Region. FACCE MACSUR Rep. 2014, 3, 3–58. [Google Scholar]
  103. Liáng, L.L.; Kirschbaum, M.U.F.; Giltrap, D.L.; Wall, A.M.; Campbell, D.I. Modelling the Effects of Pasture Renewal on the Carbon Balance of Grazed Pastures. Sci. Total Environ. 2020, 715, 136917. [Google Scholar] [CrossRef] [PubMed]
  104. Giltrap, D.L.; Kirschbaum, M.U.F.; Liáng, L.L. The Potential Effectiveness of Four Different Options to Reduce Environmental Impacts of Grazed Pastures. A Model-Based Assessment. Agric. Syst. 2021, 186, 102960. [Google Scholar] [CrossRef]
  105. Puche, N.J.B.; Kirschbaum, M.U.F.; Viovy, N.; Chabbi, A. Potential Impacts of Climate Change on the Productivity and Soil Carbon Stocks of Managed Grasslands. PLoS ONE 2023, 18, e0283370. [Google Scholar] [CrossRef] [PubMed]
  106. Ehrhardt, F.; Soussana, J.-F.; Bellocchi, G.; Grace, P.; McAuliffe, R.; Recous, S.; Sándor, R.; Smith, P.; Snow, V.; de Antoni Migliorati, M.; et al. Assessing Uncertainties in Crop and Pasture Ensemble Model Simulations of Productivity and N2O Emissions. Glob. Chang. Biol. 2018, 24, e603–e616. [Google Scholar] [CrossRef] [PubMed]
  107. Kirschbaum, M.U.F.; Rutledge, S.; Kuijper, I.A.; Mudge, P.L.; Puche, N.; Wall, A.M.; Roach, C.G.; Schipper, L.A.; Campbell, D.I. Modelling Carbon and Water Exchange of a Grazed Pasture in New Zealand Constrained by Eddy Covariance Measurements. Sci. Total Environ. 2015, 512–513, 273–286. [Google Scholar] [CrossRef]
  108. Giltrap, D.L.; Kirschbaum, M.U.F.; Laubach, J.; Hunt, J.E. The Effects of Irrigation on Carbon Balance in an Irrigated Grazed Pasture System in New Zealand. Agric. Syst. 2020, 182, 102851. [Google Scholar] [CrossRef]
  109. Liang, L.L.; Campbell, D.I.; Wall, A.M.; Schipper, L.A. Nitrous Oxide Fluxes Determined by Continuous Eddy Covariance Measurements from Intensively Grazed Pastures: Temporal Patterns and Environmental Controls. Agric. Ecosyst. Environ. 2018, 268, 171–180. [Google Scholar] [CrossRef]
  110. Vogeler, I.; Kluß, C.; Peters, T.; Taube, F. How Much Complexity Is Required for Modelling Grassland Production at Regional Scales? Land 2023, 12, 327. [Google Scholar] [CrossRef]
  111. Sándor, R.; Barcza, Z.; Acutis, M.; Doro, L.; Hidy, D.; Köchy, M.; Minet, J.; Lellei-Kovács, E.; Ma, S.; Perego, A.; et al. Multi-Model Simulation of Soil Temperature, Soil Water Content and Biomass in Euro-Mediterranean Grasslands: Uncertainties and Ensemble Performance. Eur. J. Agron. 2017, 88, 22–40. [Google Scholar] [CrossRef]
  112. Ruelle, E.; Hennessy, D.; Delaby, L. Development of the Moorepark St Gilles Grass Growth Model (MoSt GG Model): A Predictive Model for Grass Growth for Pasture Based Systems. Eur. J. Agron. 2018, 99, 80–91. [Google Scholar] [CrossRef]
  113. Selbie, D.R.; Buckthought, L.E.; Shepherd, M.A. Chapter Four—The Challenge of the Urine Patch for Managing Nitrogen in Grazed Pasture Systems. In Advances in Agronomy; Sparks, D.L., Ed.; Academic Press: Cambridge, MA, USA, 2015; Volume 129, pp. 229–292. [Google Scholar]
  114. Homburger, H.; Lüscher, A.; Scherer-Lorenzen, M.; Schneider, M.K. Patterns of Livestock Activity on Heterogeneous Subalpine Pastures Reveal Distinct Responses to Spatial Autocorrelation, Environment and Management. Mov. Ecol. 2015, 3, 35. [Google Scholar] [CrossRef] [PubMed]
  115. Donovan, M.; Monaghan, R. Impacts of Grazing on Ground Cover, Soil Physical Properties and Soil Loss via Surface Erosion: A Novel Geospatial Modelling Approach. J. Environ. Manag. 2021, 287, 112206. [Google Scholar] [CrossRef] [PubMed]
  116. Harrison, M.T.; Cullen, B.R.; Rawnsley, R.P. Modelling the Sensitivity of Agricultural Systems to Climate Change and Extreme Climatic Events. Agric. Syst. 2016, 148, 135–148. [Google Scholar] [CrossRef]
  117. Buisan, S.T.; Saz, M.A.; López-Moreno, J.I. Spatial and Temporal Variability of Winter Snow and Precipitation Days in the Western and Central Spanish Pyrenees. Int. J. Climatol. 2015, 35, 259–274. [Google Scholar] [CrossRef]
  118. Aquilani, C.; Confessore, A.; Bozzi, R.; Sirtori, F.; Pugliese, C. Review: Precision Livestock Farming Technologies in Pasture-Based Livestock Systems. Animal 2022, 16, 100429. [Google Scholar] [CrossRef]
  119. Michez, A.; Lejeune, P.; Bauwens, S.; Herinaina, A.A.L.; Blaise, Y.; Castro Muñoz, E.; Lebeau, F.; Bindelle, J. Mapping and Monitoring of Biomass and Grazing in Pasture with an Unmanned Aerial System. Remote Sens. 2019, 11, 473. [Google Scholar] [CrossRef]
  120. Insua, J.R.; Utsumi, S.A.; Basso, B. Estimation of Spatial and Temporal Variability of Pasture Growth and Digestibility in Grazing Rotations Coupling Unmanned Aerial Vehicle (UAV) with Crop Simulation Models. PLoS ONE 2019, 14, e0212773. [Google Scholar] [CrossRef] [PubMed]
  121. Greenwood, P.L.; Paull, D.R.; McNally, J.; Kalinowski, T.; Ebert, D.; Little, B.; Smith, D.V.; Rahman, A.; Valencia, P.; Ingham, A.B.; et al. Use of Sensor-Determined Behaviours to Develop Algorithms for Pasture Intake by Individual Grazing Cattle. Crop Pasture Sci. 2017, 68, 1091–1099. [Google Scholar] [CrossRef]
  122. Ash, A.; Hunt, L.; McDonald, C.; Scanlan, J.; Bell, L.; Cowley, R.; Watson, I.; McIvor, J.; MacLeod, N. Boosting the Productivity and Profitability of Northern Australian Beef Enterprises: Exploring Innovation Options Using Simulation Modelling and Systems Analysis. Agric. Syst. 2015, 139, 50–65. [Google Scholar] [CrossRef]
Table 1. Summary of the analyzed models.
Table 1. Summary of the analyzed models.
ModelTypeGrassland
Calibrated
Area of StudyReferences
APSIMAgriculturalYesEurope, Oceania[52,53,54,55,56,57,58,59,60]
STICSAgriculturalNoEurope, North America[61,62,63,64,65,66,67]
LINGRAAgriculturalYesEurope[68,69,70,71,72,73,74]
CROPSYSTAgriculturalNoEurope[75,76,77,78,79,80,81]
WOFOSTAgriculturalNoChina, Europe[82,83,84,85,86,87,88]
PaSIMBiogeochemicalYesEurope[89,90,91,92,93,94,95]
Biome-BCGBiogeochemicalYesChina, Europe, North America[96,97,98,99,100,101,102]
CenWBiogeochemicalYesEurope, Oceania, North America[103,104,105,106,107,108,109,110]
Table 2. Parameters included in the models.
Table 2. Parameters included in the models.
ModelMowingGrazingBiodiversityFertilizationAmount of Data Required
APSIMYesYesYesYesMedium
STICSNoYesNoYesMedium
LINGRANoYesNoYesLow
CROPSYSTNoYesNoYesMedium
WOFOSTNoNoNoYesLow
PaSIMYesYesYesNoHigh
Biome-BCGYesYesYesNoHigh
CenWNoNoYesNoHigh
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Jarne, A.; Usón, A.; Reiné, R. Predictive Production Models for Mountain Meadows: A Review. Agronomy 2024, 14, 830. https://doi.org/10.3390/agronomy14040830

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Jarne A, Usón A, Reiné R. Predictive Production Models for Mountain Meadows: A Review. Agronomy. 2024; 14(4):830. https://doi.org/10.3390/agronomy14040830

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Jarne, Adrián, Asunción Usón, and Ramón Reiné. 2024. "Predictive Production Models for Mountain Meadows: A Review" Agronomy 14, no. 4: 830. https://doi.org/10.3390/agronomy14040830

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