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# Application of machine learning techniques to simulate the evaporative fraction and its relationship with environmental variables in corn crops

*Ecological Processes*
**volume 11**, Article number: 54 (2022)

## Abstract

### Background

The evaporative fraction (EF) represents an important biophysical parameter reflecting the distribution of surface available energy. In this study, we investigated the daily and seasonal patterns of EF in a multi-year corn cultivation located in southern Italy and evaluated the performance of five machine learning (ML) classes of algorithms: the linear regression (LR), regression tree (RT), support vector machine (SVM), ensembles of tree (ETs) and Gaussian process regression (GPR) to predict the EF at daily time step. The adopted methodology consisted of three main steps that include: (i) selection of the EF predictors; (ii) comparison of the different classes of ML; (iii) application, cross-validation of the selected ML algorithms and comparison with the observed data.

### Results

Our results indicate that SVM and GPR were the best classes of ML at predicting the EF, with a total of four different algorithms: cubic SVM, medium Gaussian SVM, the Matern 5/2 GPR, and the rational quadratic GPR. The comparison between observed and predicted EF in all four algorithms, during the training phase, were within the 95% confidence interval: the *R*^{2} value between observed and predicted EF was 0.76 (RMSE 0.05) for the medium Gaussian SVM, 0.99 (RMSE 0.01) for the rational quadratic GPR, 0.94 (RMSE 0.02) for the Matern 5/2 GPR, and 0.83 (RMSE 0.05) for the cubic SVM algorithms. Similar results were obtained during the testing phase. The results of the cross-validation analysis indicate that the *R*^{2} values obtained between all iterations for each of the four adopted ML algorithms were basically constant, confirming the ability of ML as a tool to predict EF.

### Conclusion

ML algorithms represent a valid alternative able to predict the EF especially when remote sensing data are not available, or the sky conditions are not suitable. The application to different geographical areas, or crops, requires further development of the model based on different data sources of soils, climate, and cropping systems.

## Background

Intensive agricultural systems in the Mediterranean areas represent the largest consumers of fresh water and, in some cases, threatening the availability of water resources for other uses (Nguyen et al. 2016; Alexandridis et al. 2009). Projections of future climate change indicate an increasing pressure on water use in the Mediterranean regions as consequence of progressive increase in global temperatures and many countries of this area have already experienced water shortages during the last 20 years (Milano et al. 2013).

Several methodologies are currently available to measure the water use in agricultural systems: among them, the direct observation of the evapotranspiration or latent heat flux (LE) using the eddy covariance (EC) technique at ecosystem level, represents the most widely used approach worldwide (Baldocchi 2020). LE is a key component of the energy, carbon, and hydrological cycle: several land surface processes are tightly linked to evapotranspiration through complex feedback mechanisms, such as precipitation (Zveryaev and Allan 2010), surface temperature (Seneviratne et al. 2006), available energy (Gentine et al. 2011) and the amount of soil water available for the plants (de Tomás et al. 2014).

The evaporative fraction (EF), defined as the ratio between LE and the sum of LE and sensible heat flux (*H*), represents an important biophysical parameter reflecting the distribution of surface available energy, and a good tool for interpreting the components of the energy budget (Gentine et al. 2011). In terms of ecophysiological processes, EF is coupled to drought events (Schwalm et al. 2010; Trenberth and Guillemot 1996): when EF approaches unity, most of the available energy is partitioned to LE and water can flow without limitations through the soil–plant–atmosphere continuum; therefore, EF can be viewed as an index of water deficit, ranging from 0, when no water is available, to 1 when there are no water limitations (Schwalm et al. 2010). Several studies investigated the EF of cropland in the last decade. Zhou and Wang (2016) reported a positive correlation between monthly EF, air temperature, NDVI and relative humidity across a network of Ameriflux sites in North America. Yang et al. (2013) analyzed the diurnal patterns of EF, indicating that the self-preservation assumption no longer holds over growing seasons, and diurnal patterns of evapotranspiration are mainly influenced by stomatal regulation. The EF has also been used to predict the evapotranspiration (ET) from remotely sensed instantaneous observations by the application of an improved constant EF Method that include the use of a decoupling factor (*Ω*) to represents the relative contribution of the radiative and aerodynamic terms to the overall ET (Tang et al. 2017a) or from remotely sensed real time observations with a simplified derivations of a theoretical model (Tang et al. 2017b).

The analysis of daily behavior of EF and its response to biophysical factors have been investigated by Gentine et al. (2011), showing that it is rarely constant and that its temporal power spectrum is wide. EF can either be derived from micrometeorological observations (Schwalm et al. 2010), satellite products such as MODIS (Nutini et al. 2014; Lu et al. 2013a) or from empirical models based on satellite observations and functional relationships (Zhou and Wang 2016). Ground-based observations of EF are normally conducted within experimental observation network such as Fluxnet, ICOS and NEON. Over the past decades the increasing number of geoscientific, atmosphere, and land surface data availability from the research network infrastructures, have co-evolved with development of new machine learning (ML) algorithms (Reichstein et al. 2019).

ML is currently used to simulate a wide range of biophysical and environmental processes, and has been rapidly expanding, covering a wide range of scientific disciplines. ML can be defined as the subset of Artificial Intelligence that provides computer systems the ability to simulate human intelligence (Dash et al. 2021). In recent years ML has been applied in more and more scientific fields including, for example, bioinformatics (Kong et al. 2007), biochemistry (Richardson et al. 2016; Wildenhain et al. 2015), medicine (Kang et al. 2015), meteorology (Kramer et al. 2017; Aybar-Ruiz et al. 2016), economic sciences (Barboza et al. 2017), robotics (Takahashi et al. 2017), aquaculture (López-Cortés et al. 2017), and climatology (Fang et al. 2017). The supervised ML can be classified in two main groups: “classification model” where the target variables are categories, and “regression model” where predictor and target are continuous variables (Liakos et al. 2018). Regression models are among the hottest topics in the development of algorithms able to learn from data and build predictions without being explicitly parameterized for that task. This makes the models able to predict future outcomes after being trained on the basis of past experimental observations where predictor variables are used to train the model with the aim of producing a function that is approximate enough to be able to predict an output (target variables) from new inputs when they are introduced (Sen et al. 2020).

Over the last few years, literature related to the use of ML in agricultural sciences has been growing significantly, and several efforts to predict the energy balance components have been made: Zhao et al. (2019) developed a physics-constrained ML model, able to predict the ET across a series of Fluxnet sites; a similar study was conducted by Tramontana et al. (2016) where several ML methods were used to predict CO_{2} and energy exchange (i.e., LE and *H*) across multiple Fluxnet sites. More recently, Pan et al. (2020) used an ensemble of remote sensing, ML and land surface modeling to simulate the ET at global level, while Mosre and Suárez (2021) report the use of ML with in situ remote sensing data to determine the actual ET in arid cold regions. ML algorithms have been also used to predict CO_{2} (Guevara-Escobar et al. 2020), latent heat flux (Zhao et al. 2019; Dou and Yang 2018; Yin et al. 2021; Fu et al. 2021; Mosre and Suárez 2021), reference evapotranspiration (Anurag et al. 2021; Borges et al. 2020), and to evaluate terrestrial evapotranspiration at global scale (Pan et al. 2020).

Nevertheless, to our best knowledge, there is still a lack of ML application to predict the daily EF for agricultural crops in Mediterranean regions. The application of new methods to determine EF could represent a valid alternative to conventional remote sensing-based models, especially when the sky conditions are unsuitable, or data are not available. The aim of this study is, therefore, to investigate the daily and seasonal patterns of EF on a multi-year corn cultivation located in southern Italy and evaluate the performance of different ML algorithms to predict the EF at daily time step. In this study, instead of choosing one particular model, we have first trained our dataset to several ML models in parallel, and then we have chosen to develop only the models with the higher performances.

## Methods

### Experimental site

Data collection occurred during the period 2004–2009 on a farm located in southern Italy (40° 31′ 25.5″ N, 14° 57′ 26.8″ E) that is the European southernmost cropland observation candidate site of the ICOS (Integrated Carbon Observation System) European infrastructure. The area is characterized by typical Mediterranean climate: over the last 30 years, the average annual precipitation was 908 mm with an overall mean air temperature of 15.5 °C. Most of the precipitation occurs in October–November while the driest month is July. The site was cultivated with silage corn (*Zea mays*) as main crop; the vegetative season was defined according to its growing cycle (i.e., day of sowing, and day of harvest).

The site was equipped with an EC system composed of a fast response sonic anemometer (R3, Gill Instruments Ltd., Lymington, UK) and open-path infrared CO_{2}/H_{2}O gas analyzer (Li-7500, Li-Cor Inc., Lincoln, NE, USA) to measure energy fluxes (Latent Heat Flux, LE and Sensible Heat Flux, *H*) and the CO_{2} net ecosystem exchange (NEE). More detailed information about the EC system and ancillary sensors can be found in Vitale et al. (2007) and Vitale et al. (2016). To achieve a satisfactory upwind fetch, the height of eddy covariance sensors was set to 2 m above the ground while the canopy was shorter than 1 m and later moved following the crop growth up to 3.9 m at harvest time. The experimental field covers an area of 10 ha, whereas the average footprint was 182 m along the prevalent wind direction (NE–SW).

Data streams from both IRGA and sonic anemometer were logged at a frequency of 20 Hz via the Eddymeas software, and the fluxes calculated using the software EddySoft (Kolle and Rebmann 2007). Corrections for flux losses as well as for sensor separation (Horst and Lenschow 2009) and low-pass frequency filters (Moncrieff et al. 2004) were also applied. High-frequency spectral correction was performed according to the model of Eugster and Senn (1995). The flux footprint was computed according to the analytical model of Schuepp et al. (1990), and quality control was applied to half-hourly (30-min) fluxes following Göckede et al. (2004), by assigning a quality flag (0 for good data, 1 for acceptable data, 2 for bad data) to each flux value. The standard WPL terms were considered to correct for density fluctuations (see Webb et al. 1980).

EC data used in this study were part of the Fluxnet 2015 Dataset (https://fluxnet.org/data/fluxnet2015-dataset/). Time series were processed according to the approaches reported in Pastorello et al. (2020). This methodology includes a preliminary processing block, where data quality assurance and quality control (QA/QC) for all the variables investigated are carried out by means of a variable-specific despiking routines. Energy fluxes (*H* and LE), used in this study were then gap-filled using the MDS method (Reichstein et al. 2005) and the values were adjusted according to a methodology that corrects for un-closure of the energy budget, by assuming a correct Bowen ratio. The corrected fluxes are obtained by multiplying the original, gap-filled LE and *H* data by an energy balance closure correction factor (EBC_CF), which is calculated on a subset of observations—where all the components needed to calculate the energy balance closure are available—namely: measured net radiation (*R*_{n}) and soil heat flux (*G*), and measured or good-quality gap-filled latent heat and sensible heat fluxes. The correction factor is calculated for each half-hour as (*R*_{n} – *G*) / (*H* + *LE*), and the time series is filtered removing the values that are outside 1.5 times the interquartile range, then used as a basis to calculate the corrected *H* and LE fluxes.

Environmental variables were measured at 1 Hz and averaged every half-hour: precipitation was monitored using a rain gauge (Rain Collector II, Davis Instruments, CA, USA) located on the ground, soil temperature and volumetric water content (SWC) at 0.3-m depth were also determined by means of TCAV, 105E thermocouple probes and CS 616 water content reflectometer (Campbell Scientific, Ltd., Shepshed, UK), respectively.

Soil heat flux density was monitored with heat flux plates (HFT3 Campbell Sci. Ltd., Shepshed, UK) at 5 cm below the soil surface. Data were collected at three different locations within the footprint area of the EC tower and with a time step of 30 min. *G* values coming from the plate were first corrected for the change in heat storage in the soil layer above the plate following the methodology reported in the Instruction for soil-meteorological measurements of the ICOS) protocol (Op de Beeck et al. 2017).

The main components of the solar radiation, i.e., incoming, reflected and net radiation, were monitored using an Eppley pyranometer (Eppley Laboratory Inc., USA) CNR1 net radiometer (Kipp & Zonen, NL), all located at 4 m from the ground, while air temperature and vapor pressure were monitored using the Bowen Ratio System (Campbell Scientific Ltd., Shepshed, UK).

Leaf area index (LAI), monitored for the entire crop cycle by sampling plants at different locations of the field to cover the spatial variability, was determined using a Li-3100 leaf area meter (Li-Cor Biosciences, Lincoln, Nebraska, USA). For the years 2008–2009, LAI data were obtained from high spatial resolution data acquired by SPOT family satellite, as the field data were too sparse. Map elaborations were based on an empirical relationship between LAI and one-view angle measurements of reflectance (rλ) in the red and infrared bands (for more specific information, see Vitale et al. 2016).

### Evaporative fraction

The partitioning of incoming energy was evaluated using the EF approach. The instantaneous EF (dimensionless) was calculated from LE (W m^{−2}) and *H* (W m^{−2}) fluxes, measured by the above-described EC station, as follows:

where the time difference *t*_{2}–*t*_{1} in the present study refers to the time from 08:00 to 18:00 (UTC + 1) (Zenone et al. 2015). An ideal energy balance closure can be achieved when the available energy is equal to the turbulent fluxes, and then, EF can be expressed as:

where *R*_{n} is the net radiation and *G* is the soil heat flux. EF is a biophysical parameter related to the partitioning of available energy and therefore to the energy balance closure at the measuring point. EC fluxes of energy typically do not satisfy the energy balance closure, due to different levels of sensor errors, unmeasured storage terms, mismatches in source area and landscape heterogeneity (Foken 2008).

To overcome this issue, EF can be rewritten as

We could then assume that the errors on LE and *H* present similar magnitude (Hollinger and Richardson 2005; Richardson et al. 2006; Foken 2008) and are uncorrelated; this allows to mathematically cancel out the errors linked to the lack of energy balance closure (Schwalm et al. 2010).

### Methodology flowchart adopted for the ML algorithms application

The ML methodology adopted to predict the EF using the ML algorithms consists of 3 main steps (Fig. 1):

*Step 1: Predictors selection*. A preliminary analysis was conducted to determine which input variables (Table 1) have the highest statistical significance on the prediction of EF. This involved the use of the neighborhood component analysis (NCA, see Wang and Tan 2017), the minimum redundancy maximum relevance (MRMR, see Jo et al. 2019) algorithms, and a correlation matrix to determine the Pearson coefficient as well as the variance inflation factor (VIF) to check the multicollinearity among the predictors.

*Step 2**: **Selection of the best ML algorithms*. In this second step we made a preliminary application of the different ML models to compare their performance, to then identify the best ML algorithm. This included five different classes of ML algorithms: linear regression (LR), regression trees (RT), Gaussian process regression (GPR), support vector machines (SVM), and ensembles of tree (ETs) models. The methods that provided values of *R*^{2} > 0.65 during the training process were further developed and investigated: two classes of ML algorithm were selected, the GPR and the SVM.

*Step 3: ML application*

#### GPR models

To investigate the relationship between the environmental features selected and the EF variability, a GPR model (Rasmussen and Williams 2006) was adopted. GPR model assume that the output *y* of a function f with input *x* can be expressed as

where *x* is the input vector, *f* is the function value and *y* is the observed target value.

We have supposed that the observed *y* values differ from the function values *f*(*x*) by additive noise, and we will further assume that this noise follows an independent, identically distributed Gaussian distribution with zero mean, variance \({\sigma }_{n}^{2}\) and \(\varepsilon \sim (0, {\sigma }_{n}^{2}\)).

GPR model assume also that not only the error term \(\in\), but also \(f\) is considered as a random variable (Ballabio et al. 2019). The GPR \(f(x)\) is distributed as a Gaussian process:

where *f*(*x*) is defined by its mean *μ*(*x*) and covariance *k*(*x*,*x*∗).

The covariance function *k*, is known as the kernel function of the GPR models and analyzes the dependence of the function values between different values of *x*. The kernel function of a GPR model can be considered equivalent to Kriging (Stein 1999). While Kriging is, in general, performed on a geographical space, the GPR is applied arbitrarily to a number of different covariates. The choice of the appropriate kernel function is based on the structure, or peculiar patterns of the data investigated (Ballabio et al. 2019).

In this study, two kernel functions, the Matern 5/2 (Eqs. 6, 7) and the rational quadratic (Eq. 8) were used:

where

is the Euclidean distance between *x*_{i} and *x*_{j} and *σ*_{l} is the characteristic length scale.

where *σ*_{l} is the characteristic length scale, *α* is a positive scale-mixture parameter, and

is the Euclidean distance between *x*_{i} and *x*_{j}.

It is possible to use a separate length scale *σ*_{m} for each predictor *m* (*m* = 1, 2, …,*d*).

The built-in kernel (covariance) functions with a separate length scale for each predictor implement automatic relevance determination. The unconstrained parametrization *θ* in this case is

#### SVM regression

SVM analysis is a popular machine learning tool for classification and regression, first identified by Vapnik (1999). SVM regression is considered a non-parametric technique because, as GPR, it relies on kernel functions. SVM employs a model able to build a decision surface by mapping the input and target variables into a high-dimensional (or infinite-dimensional) feature space. Next, a linear regression is executed in the high-dimensional feature space. This mapping operation is required because in many cases, the relation between a multidimensional input (i.e., predictor variables) and the output (i.e., target variables) is unknown and very likely to be nonlinear. SVM regression aims at finding a linear hyperplane, which fits the multidimensional input vectors to output values (Wauters and Vanhoucke 2014). Two SVM kernel functions, the cubic Gaussian (Eq. 12) and polynomial (Eq. 13) were used:

where *q* is in the set {2,3,…} and *G* is a Gram matrix of an *n*-by-*n* matrix that contains elements *g*_{i,j} = *G*(*x*_{i},*x*_{j}). Each element *g*_{i,j} is equal to the inner product of the predictors as transformed by *φ*. However, we do not need to know *φ*, because we can use the kernel function to generate Gram matrix directly. Using this method, nonlinear SVM finds the optimal function *f*(*x*) in the transformed predictor space.

### Quality assessment

For the evaluation of the results of the ML models, several criteria were used: the determination coefficient (*R*^{2}), root mean squared error (RMSE), mean absolute error (MAE), and mean squared error (MSE). *R*^{2} is a key output in regression analysis, while RMSE is a measure of the average squared difference between the predicted and actual outputs of a model, the MAE measures the average error between them. In contrast to *R*^{2}, lower values of RMSE and MAE indicate a better performance of an algorithm.

#### Cross-validation analysis

In the current analysis, the evaluation of ML model performance was based on EF data split into 5-year training set (2004 to 2008) and 1-year testing set (2009). However, this analysis remained only partially reliable since the predictive performance obtained for only one test set can be different to that obtained for another test set (Rodríguez et al. 2010). In order to tackle this potential issue, we apply the *K*-fold cross-validation to the original dataset; all the data collected were split into ten randomly partitioned sets (*K* = 10 folds) of almost equal size. In the first iteration, the first fold (*K* = 1) was used to test ML models and the remaining folds (*K* = 2 to 10) were used for the training. In the next iteration, the second fold (*K* = 2) served for the testing stage, while the rest (*K* = 1 and *K* = 3 to 10) were used for the training. The process was repeated until the final iteration was reached.

## Results

Based on the growing seasons full datasets, average diurnal cycles of LE + *H*, *H* and EF were calculated for each month, as shown in Fig. 2. Heat fluxes show the typical Gaussian shape, whereas EF features a characteristic concave U profile, with higher values in the early morning (e.g., 0.7–0.8 for July and August) and late afternoon hours while lower values (e.g., 0.4–0.5) were observed in late spring (May), early summer (June) and early fall (September). Considering only data spanning across midday (i.e., from 11:00 to 13:00), the EF behavior appears to be more constant demonstrating a little variance of the daytime values, with the average values ranging between 0.4 and 0.6, during the entire growth cycle.

### Step 1: predictors selection

The correlation matrix reported in Table 2 indicated, as expected, a significant correlation between several of the predictors as indicated by the *p* values < 0.05. The correlation between the predictors and EF were all significant and the highest correlation was found between EF and *G* (*R* = 0.40, *σ* = 4 × 10^{–10}). The VIF indicates an average value among all the predictors of 1.858 and a collinearity tolerance of 0.580. The results from the other two feature selection methods, i.e., NCA and MRMR are illustrated in Fig. 3: both methodologies identified LAI and *R*_{n} as predictors with the lowest weight (close to zero). The feature weights obtained from the NCA analysis suggested that (classified from highest to lowest values) air temperature (*T*_{a}), NEE, SWC, *G* and VPD were the most influencing factors on EF predictions (Fig. 3B). The feature weights obtained from the MRMR partially confirmed the NCA results, indicating NEE, *T*_{a}, and *G* as the main predictors, while VPD and SWC score was close to zero (Fig. 3A). In view of these findings, NEE, SWC, *T*_{a}, VPD, and *G* were selected for the ML predictive analysis on EF prediction: NEE represents the net CO_{2} exchange between the ecosystem and the atmosphere, measured with the EC technique, to emphasize the role of the gas exchange, the volumetric SWC representing the amount of water potentially available for the vegetation, the *T*_{a} and VPD represents the atmospheric physical conditions, and *G* is component of the energy balance of the ecosystem investigated.

### Selection of the best ML algorithm

The results from the different ML algorithms proposed for the training phase are shown in Table 3, in terms of the different evaluation criteria adopted (see “Quality assessment” section). The linear regression models among the four methods (see Table 3) show an average *R*^{2} of 0.44 (± 0.06) and an average RMSE of 0.1 (± 0.005), while for the regression tree group *R*^{2} was 0.41 (± 0.05) and RMSE 0.19 (± 0.005). Similar results were found for the SVM model, with an average *R*^{2} of 0.44 (± 0.11) and RMSE of 0.01 (± 0.002), while slightly better performance was found for the ensemble of tree models: *R*^{2} 0.54 (± 0.15) and RMSE 0.009 (± 0.002). The best performances were found for two algorithms: cubic Gaussian SVM (Eq. 9) and polynomial (Eq. 10) SVM classes; and the Matern 5/2 (Eq. 6) and rational quadratic (Eq. 7) GPR classes. The results of the training-and-testing phase instead are reported in Table 4.

### ML application

The results from the application of the selected 4 ML on the training phase are shown in Fig. 4, where the time series of daily EF values are plotted; the values of the EF, for the all years considered in the study, ranged from 0.07 to 0.74: the comparison between observed and predicted EF shows that for all 4 models the predicted values were within the 95% confidence interval: with an average *R*^{2} among the ML algorithms of 0.88 (± 0.1). The *R*^{2} and RMSE obtained for each ML model are reported in Fig. 4.

The results of the testing phase are shown instead in Fig. 5: the average *R*^{2} between observed and predicted daily EF of 0.66 (± 0.06). The results of the cross-validation analysis (see “Cross-validation analysis” section) are reported in Table 5: the *R*^{2} obtained among all the iterations for each of the 4 adopted ML algorithms were fundamentally constant with a very narrow range between the min and max *R*^{2} obtained.

The results confirm the superiority of the GPR rational quadratic model, as indicated by the highest *R*^{2} and lowest RMSE values, compared to the other ML models.

## Discussion

The different components of the land surface energy balance follow the diurnal trend of the incoming radiation forcing with different amplitude and phase characteristics (Gentine et al. 2011). The EF is considered as a diagnostic of the surface energy balance and is rarely constant during daytime (Gentine et al. 2011). Daytime self-preservation of the EF is mainly due to the high level of solar radiation around midday, while it is sensitive to the presence of warm and dry air above the atmospheric boundary layer (Gentine et al. 2011), typical of drought periods and therefore has been used as water deficit index (Hu et al. 2019; Schwalm et al. 2010) or to determine the daily evapotranspiration (Liu et al. 2020). Water availability increases EF values (Lhomme and Elguero 1999; Schwalm et al*.* 2010), and under concurrent conditions of a cloudless sky, it contributes to daily trends of EF featuring a typical concave shape. On the other hand, when water is the limiting factor, an enhancement of EF in the late afternoon is often found from field studies (Gentine et al. 2007).

It is generally accepted (Zhou and Wang 2016; Liu et al. 2019; Liu et al. 2020, Peng et al. 2013) to refer operationally to EF_{daytime}, i.e., the EF determined during daylight hours: considering that LE and *H* are near zero during nighttime, the estimated EF values can fluctuate greatly and can therefore be of little practical use. Moreover, during the transition periods from daytime to nighttime, the hourly EF is likely to be very unstable, and most of the times it fluctuates abruptly. For this reason, only EF_{daytime} values were considered and simulated in this study.

When not available from direct observation, the EF is commonly simulated using a wide range of remote-sensing-based modeling schemes that have been proposed over past few decades, and goes from simple empirical formulas to complex land surface process models (Norman et al. 1995; Bastiaanssen et al. 1998; Su 2002; Nishida et al. 2003; Allen et al. 2007; Anderson et al. 2007; Mu et al. 2007; Bateni et al. 2013; Xu et al. 2014). Moreover, several studies have documented the advantages of the surface temperature-vegetation index method, and its applicability in the estimation of EF has been tested in several different regions across the world. (Rahimzadeh-Bajgiran et al. 2012; Yang et al. 2015; Liu et al. 2017; Hu et al. 2018; Carlson and Petropoulos 2019).

Our results demonstrate a potential for using ML to predict the EF. When tested against 6 years of EF measurements, the selected ML models were able to explain up to 99% (on the best case, and 81% on average) of the observed variability of the daily EF values.

When compared to ground observations of EC measurements, the remote-sensing-based EF model showed results comparable with the ML algorithms proposed in our study. Peng and Loew (2014) reported, for cropland sites, an *R*^{2} ranging from 0.84 to 0.79 between observed and MODIS-TOA EF. Lu et al. (2013b) developed a method for estimating daily EF derived by day–night differences in surface temperature, air temperature, and net radiation showing a good agreement with measurements from an EC system corrected by the residual energy method with an *R*^{2} of 0.857. Zhu et al. (2020) proposed a revised version of the surface temperature-vegetation index to retrieve simultaneously soil moisture and EF, showing an *R*^{2} around 0.70 between observed and estimated EF. Remote-sensing-based EF models can therefore be considered the most widely used methodology to derive EF, especially as they allow the estimate at different spatio-temporal scales, including areas not covered by experimental network sites (Zhu et al. 2020); however, they require complex parameterization schemes and clear sky conditions which are not always achievable. The comparable performance of the ML algorithms proposed in our study with conventional remote-sensing-based EF models shows the potential of ML algorithms as a valid alternative to the conventional remote-sensing models.

The ability of ML algorithms to predict any target variable depends on the functional relationships between predictor variables and the target variable itself, as learned from the data rather than depending on an underlying process-level understanding (Breiman 2001). The ability of ML algorithms to predict the target variable (in our case, EF), is therefore correlated with the input variables available (in our case NEE, SWC, *T*_{a}, VPD and *G*). This introduces a potential limit in predicting the effects of novel conditions, which instead does not affect conventional models, with their ability to reproduce complex biophysical interactions. Nevertheless, ML algorithms might prove very useful when remote sensing data are not available. Indeed, in the ML models used in this study, key predictor variables are few (see Table 1): two weather variables (*T*_{a} and VPD), one component of the energy balance (*G*), SWC, and CO_{2} NEE. All these factors are well known drivers of EF, and conventionally measured in experimental sites within research infrastructure networks, such as ICOS, Fluxnet, NEON and LTER.

Previous studies by Williams et al. (2015) and Puma et al. (2013) focused on the influence of vegetation on EF showing that the state of the crop canopy (e.g., LAI) exercises a stronger control on EF than SWC, and that LAI variability led to seasonal differences in LE and *H*, and thus EF. Bagley et al. (2017) report that differences in LAI between winter wheat and grassland/pasture led to differences in LE and *H*, and therefore on the magnitude of the observed EF. In our study, the application of both the neighborhood component analysis and the minimum redundancy maximum relevance indicate a negligible contribution of LAI as predictor, and therefore it was not included among the predictor variables. Moreover, including the LAI among the predictors resulted only in a limited improvement on the ML models: in particular the *R*^{2} increased from 0.72 to 0.77 for the GPR Matern 5/2; from 0.75 to 0.79 for the GPR Rational quadratic; from 0.68 to 0.71 for the polynomial SVM; for the cubic Gaussian SVM instead, we observed a reduction of the *R*^{2} from 0.72 to 0.67 (data not shown). Another important variable, able to predict up to 40% of the EF variability is the normalized difference vegetation index (NDVI), as reported by Zhou and Wang (2016) in a study over a series of agricultural sites within the Ameriflux network. In this study, we have intentionally avoided using NDVI, or other predictors that cannot be easily measured at site level from conventional meteorological observations, in the attempt to produce a simple model to predict the EF from field observations.

While our challenge was to test the ML models ability to reliably reproduce the EF at a specific site, it would be naïve to believe that the proposed ML algorithms from this study might be successfully applied to different soils, climates, or crop production systems considering that they were trained only on a dataset from a single corn crop site. Further research in this direction should focus on analyses including multiple sites across different terrestrial ecosystems, in order to extend the applicability of ML algorithms to effectively predict the EF.

## Conclusions

From this study, daily EF predictions have been reliably derived for a corn crop in a Mediterranean region using ML algorithms. The application to other geographical areas and crops requires further improvements, applying model training based on diverse data sources from different soils, climate, cropping systems and agronomic managements. Our results show that support vector machine and Gaussian process regression algorithms are able, with limited input measurement data, to explain a substantial portion of the EF variability. The performance of the tested ML algorithms has proven to be comparable to the conventional remote sensing-based models and can be used when the sky conditions are not suitable for remote sensing observations. In addition, ML algorithms facilitate the interpretation of interactions between the predictors and the EF. Our results also suggest that in principle the integration of ML algorithms with remote sensing-based models could be an opportunity to improve the predictability of EF.

## Availability of data and materials

Data are available upon reasonable request.

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## Acknowledgements

The authors thank Dr Paul di Tomasi for the technical support of the EC instrumentation, and Dr Andrea Esposito for the informatic support of the data acquisition. We thank also Mr Gaetano and Lazzaro Jemma owners of the “Jemma farm” who hosted our experimental EC installation

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The study was conducted under the aegis of the European Integrated Carbon Observation System (ICOS).

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TZ: analyzed the data and wrote the manuscript; DF: reviewed the manuscript and provided the data; LV: reviewed the manuscript; VM: reviewed the manuscript. All authors read and approved the final manuscript.

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Zenone, T., Vitale, L., Famulari, D. *et al.* Application of machine learning techniques to simulate the evaporative fraction and its relationship with environmental variables in corn crops.
*Ecol Process* **11**, 54 (2022). https://doi.org/10.1186/s13717-022-00400-1

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DOI: https://doi.org/10.1186/s13717-022-00400-1