Faced with environmental degradation, governments worldwide are developing policies to safeguard ecosystem services (ES). Many ES models exist to support these policies, but they are generally poorly validated, especially at large scales, which undermines their credibility. To address this gap, we describe a study of multiple models of five ES, which we validate at an unprecedented scale against 1675 data points across sub-Saharan Africa. We find that potential ES (biophysical supply of carbon and water) are reasonably well predicted by the existing models. These potential ES models can also be used as inputs to new models for realised ES (use of charcoal, firewood, grazing resources and water), by adding information on human population density. We find that increasing model complexity can improve estimates of both potential and realised ES, suggesting that developing more detailed models of ES will be beneficial. Furthermore, in 85% of cases, human population density alone was as good or a better predictor of realised ES than ES models, suggesting that it is demand, rather than supply that is predominantly determining current patterns of ES use. Our study demonstrates the feasibility of ES model validation, even in data-deficient locations such as sub-Saharan Africa. Our work also shows the clear need for more work on the demand side of ES models, and the importance of model validation in providing a stronger base to support policies which seek to achieve sustainable development in support of human well-being.
We validate multiple ecosystem services (ES) models across sub-Saharan Africa (SSA)
We find that more complex ES models sometimes provide more accurate estimates
Realised use of ES is closely aligned with human population density (demand) in SSA
Ecosystem services (ES)—nature’s contributions to people (Pascual and others 2017)—are of global importance to human well-being, but are increasingly threatened by human activities (Steffen and others 2015). As a result, many governments are now moving to ES-based management of natural resources (Wong and others 2014) and 132 United Nation member states have signed up to the Intergovernmental Science-Policy Platform for Biodiversity and Ecosystem Services (IPBES; www.ipbes.net). This shift in policy requires accurate spatial modelling of ES (Malinga and others 2015), as managing ES requires an understanding of their spatial distribution and heterogeneity (Swetnam and others 2011; Spake and others 2017) and the ability to project and compare the outcomes of management scenarios (Willcock and others 2016). Models can provide credible information where empirical ES data are sparse, which is especially the case in many developing countries (Suich and others 2015).
To meet demand for an enhanced understanding of ES flows, many spatial modelling methods and tools for mapping ES have been developed, ranging from very simple land cover-based proxies to sophisticated process-based models (IPBES 2016). Whilst a growing literature is comparing the outputs and features of the different tools (Bagstad and others 2013; Turner and others 2016), validation of these models is challenging and thus rare in the literature (Bennett and others 2013). Few studies have validated single ES models against independent datasets and then only rarely at a larger, country scales (Mulligan and Burke 2005; Bruijnzeel and others 2011; Redhead and others 2016, 2018). Even more rare are studies that explicitly validate multiple ES models simultaneously, and these generally involve small areas at catchment scale (Sharps and others 2017). As a consequence, the uncertainties associated with most ES models and the datasets that underpin them remain largely unknown (Bryant and others 2018; van Soesbergen and Mulligan 2018). This is a particular issue as the results of local-scale validation are likely not to be transferable to new locations (Redhead and others 2016) or to the regional and national scales at which ES model outputs are most widely used (Willcock and others 2016). As a result, attempts at validation by those applying models in new settings are all the more important (Bryant and others 2018). Indeed, rescaling social–ecological patterns and processes to different spatial resolutions and extents can induce substantial systematic bias (Grêt-Regamey and others 2014), providing challenges to decision-making in situations where model results are the only source of information. Lack of proven credibility, salience and legitimacy are the major reasons for the ‘implementation gap’ between all ES research (not just ES models) and its incorporation into policy- and decision-making (Cash and others 2003; Voinov and others 2014; Wong and others 2014; Clark and others 2016).
Approaches to improve the reliability of model predictions in general include increasing model complexity [defined here as model structural complexity (Kolmogorov 1998), sometimes also referred to as model complicatedness (Sun and others 2016)]. Computational capacity has rapidly increased over time, enabling ES models to become more complex and multiple models to be run at higher resolutions across larger spatial ranges (Levin and others 2013). However, increasing the complexity of ecological models typically also increases the amount of data and expertise required for implementation and interpretation, with unclear consequences for the results (Merow and others 2014). In short, it is unclear whether an investment in increasing model complexity leads to more accurate information for policy- and decision-making on local and regional scales.
The unknown credibility of ES models (Voinov and others 2014) is most pronounced where they are arguably most needed—in many developing countries, where data collection and model development efforts are least advanced (Suich and others 2015). Such ES information is important because the rural and urban poor are often the most dependent on ES (either directly or indirectly (Cumming and others 2014)), both for their livelihoods (Daw and others 2011; Suich and others 2015) and as a coping strategy for buffering shocks (Shackleton and Shackleton 2012). A major barrier to the understanding and management of these benefit flows to the poor is a lack of information on the potential supply and realised use of ES, particularly in the developing world (Wong and others 2014; Willcock and others 2016; Cruz-Garcia and others 2017). Indeed, the comparisons of ES models to primary data that do exist are all focused on potential and not realised ES (that is, biophysical supplies only and not actual use by beneficiaries) (Bagstad and others 2014). Analyses need to be disaggregated to focus on how people use ES, from which ecosystems, and how such benefits contribute to the people’s well-being (Daw and others 2011; Bagstad and others 2014; Cruz-Garcia and others 2017).
In this paper, we validate ES models against measured ES data extending over 36 countries in sub-Saharan Africa, covering 16.7 million km2—over half of the land area of Africa—and including some of the world’s poorest regions (Handley and others 2009). We focus on five ES of high policy relevance in sub-Saharan Africa (Willcock and others 2016), and for which validation data exist in multiple locations. The potential supply of two ES (stored carbon and available water) is modelled using the existing models and a further three ES (firewood, charcoal and grazing resources) predominantly using new models generated from stored carbon outputs of the existing models. To assess ES use, we developed new standardised models for realised ES (that is, actual use by people) by weighting models of potential ES (biophysical supply) by human population density for the four measured ES where the location of beneficiaries is important (use of charcoal, firewood, grazing resources and water). We hypothesised that these new realised ES models have higher predictive power than potential ES models for these ES. We also assessed the performance of human population density alone as a predictor of ES use, as this represents the simplest possible globally available ES use model. Our rationale for doing so is that local population density is a straightforward indicator of the number of people making use of the ES, and such a simple approach for modelling realised services would be very useful if it proved to be accurate. We do not focus on comparing specific modelling platforms, as the identification of the best specific model for a particular use may shift as new models are developed and is likely be location specific: such site-specific comparisons have been done elsewhere (Bagstad and others 2013; Ochoa and Urbina-Cardona 2017). As such, our aims in this study are twofold: (1) to compare the general performance of models predicting ES supply (for stored carbon and available water) to realised ES (charcoal, firewood, grazing and water use); and (2) whether more complex ES models make better predictions.
Our approach to modelling and validation is summarised in Figure 1. We validated the existing and new—developed using outputs from the existing models (see below)—ES models against ES data, using 1675 data points from 16 independent datasets extending over sub-Saharan Africa (carbon: 214, water: 736, firewood: 285, charcoal: 59, grazing: 401; Table 1, Figure 2). We compared approaches for modelling ES ranging in complexity from simple land cover-driven production functions to process-based models (IPBES 2016). As our validation datasets vary in spatial extent and location, we accounted for the effects of spatial extent and context (Figure 1). We tested the hypotheses that ES models incorporating a more complex causal structure have higher predictive power. Since decision-makers in sub-Saharan Africa consider model complexity to mean more inputs being used to model more processes (Willcock and others 2016), we assessed model complexity in terms of the number of input variables, defining inputs as a coherent set of values covering the research area for a single feature, be it categorical or numerical (Merow and others 2014).
Description of Ecosystem Service Models
We selected ES models to test, focussing on: (1) ES models capable of estimating some of our selected potential ES (stored carbon, available water) and providing inputs to our new models of firewood, charcoal and grazing resources within our study area; (2) the subset of these models for which adequate validation data could be identified, allowing like-for-like comparisons between modelled outputs and validation data; and (3) models representing a range of complexities from simple production functions to process-based models. As such, we used six existing ES modelling frameworks that contain one or more models meeting these criteria (Table SI-1-1, SI-1-1). We selected InVEST (Kareiva 2011; McKenzie and others 2012), Co$ting Nature (Mulligan and others 2010; Mulligan 2015), WaterWorld (Mulligan 2013) and benefits transfer (based on coupling the Costanza and others (2014) values with GlobCover 2009 landcover categories; SI-1-2) due to their widespread use and global applicability (Bagstad and others 2013). We also included the well-known and partially validated (Pachzelt and others 2015) dynamic vegetation model LPJ-GUESS (Smith and others 2001, 2014). Although LPJ-GUESS is not traditionally considered an ES model and has a relatively coarse native resolution (0.5 × 0.5 degrees, but constrained mainly by the resolution of environmental input variables), it is increasingly used for ES modelling applications [including implementation within the ARIES technology (Villa and others 2014)] and it is a process-based model that gives outputs that effectively track the biophysical supply of many potential ES (Bagstad and others 2014; Lee and Lautenbach 2016). Furthermore, we included the Scholes models (comprising two grazing models and a rainfall surplus model) as it is the only large-scale ES models designed specifically for use in sub-Saharan Africa (Scholes 1998) (SI-1-3). Ideally, we would also have compared bespoke local models with local data. However, such models simply do not exist in sub-Saharan Africa in most places. Moreover, as the global models we compare run at fine spatial resolutions (except LPJ-GUESS), it is reasonable to investigate how well they perform in terms of accuracy against local data collected in many locations in many different ways (as is the case here).
At time of analysis (March 2017), InVEST, Co$ting Nature and LPJ-Guess did not have models that focus on firewood, charcoal or grazing resources, but they did explicitly output stored vegetation carbon. As the supply of these three ES is directly dependent on the amount of biomass present, which is what underpins estimates of stored vegetation carbon in all three models, we built eight new predictors using the outputs from these three existing carbon modules (to estimate the potential supply of these three additional ES (SI-1-4). These new models used spatial masks to estimate the biomass available on relevant land uses (SI-1). For example, we applied a ‘grazing’ spatial mask to derive grassland carbon from InVEST and Co$ting Nature standing carbon outputs. We excluded areas in which little to no grazing activity was expected (for example, protected areas) and included areas in which most of the above-ground carbon is assumed to be available for livestock grazing (Figure SI-1-1A; Table SI-1-5). For LPJ-Guess, we used C3/C4 carbon outputs as estimate for grazing resources. Thereafter, we converted grazing biomass to FAO livestock units for sub-Saharan Africa using the conversion factors from Houerou and Hoste (1977). Henceforth, we refer to these carbon-based predictors as ES models. Finally, we created models of realised ES by weighting models of potential ES (models of biophysical supply only; for example, the Scholes models, WaterWorld and our new models of firewood, charcoal and grazing resources) by human population (Stevens and others 2015). We also conducted like-for-like comparisons of these new models for realised use of water, firewood, charcoal and grazing resources with relative rural population data alone—the simplest possible model of ES use. We also assessed whether these new realised ES models have higher predictive power than potential ES models when compared to ES use data. We excluded urban populations for all analyses except the Poverty Environment Network usage data and water use (Table 1).
As we considered the performance of ES models separately for each ES, we did not require locations that provided primary data on all ES together. This enabled us to access 1675 data points from 16 separate validation datasets—the maximum number available to us that were suitable for the purposes of this study (that is, independent of the model calibration data; Figure 2, Table 1, SI-2). These data are diverse, being collected using a range of methods of varying reliability, including expert opinion (for example, country-level statistics from the FAO), census data (for example, district level for Kenya and Ethiopia, household level for South Africa) and biophysical measurement (for example, tree inventory plots, and weir data on water flow [both from across sub-Saharan Africa]) (Table 1). As such, each dataset has associated uncertainties (Grainger 2008) but, because the ‘true value’ can never be absolutely determined, provides acceptable reference values for validation. Given that the datasets cover a wide range of independent methods and our focus is on ranked correlative relationships between models and data, there is unlikely to be systematic bias and so data quality issues should impact our results minimally. In our analyses, some of the validation data required processing to ensure like-for-like comparison with modelled outputs. All ES models were either run at 1 × 1 km or resampled from their minimum native resolution to an exact 1 × 1 km resolution (that is, for the Scholes Firewood model [native resolution: 5 × 5 km] and for LPJ-Guess [native resolution: 55.6 × 55.6 km]). We then extracted a single summary value per polygon to align model outputs with polygon validation data (for example, each catchment for the Global Runoff Data Centre [GRDC]; each district for Kenya; each country for FAO data; see SI-2). For forest plot point validation data (the ForestPlots.net data), we compared the point data to the 1 × 1 km grid cell it was in. For the PEN data (fodder, charcoal and firewood use), we buffered the point estimate of each village location by 10 km (to align with walking distances for firewood or water (Agarwal 1983; Sewell and others 2016)) and calculated the summary value for each model for each polygon. Hence, we extracted model data to be as comparable as possible to the validation data points. This means that single values as similar in area and units as possible were extracted from each model to be compared to the single validation values as provided by the datasets listed in Table 1 (see SI-2 for full details of these methods). All data were normalised following Verhagen and others (2017) to equalise any unit differences (SI-3-3).
Calculation of Model Performance
There is no single comprehensive measure of model performance (Bennett and others 2013). Criteria commonly considered are: (1) trueness—the closeness of the agreement between the reference value and the average model value, largely affected by systematic error or bias within the model); (2) precision—the closeness of agreement between repeated model runs, largely affected by random variables or distributions that feature within the model code; and (3) accuracy—an overall summary of precision and trueness that describes the closeness of the agreement between the reference value and the values obtained from the model run(s) (IOS 1994). We focussed on accuracy and trueness here, as we only considered a single output dataset from each model (derived from a single set of parameters) and assessed these using two metrics. The first metric was the rank correlation between modelled and validation values (Spearman’s ρ)—a measure of accuracy ranging from − 1 to 1, with 1 indicating a perfect positive correlation, 0 no correlation and − 1 a perfect negative correlation. Thus, ρ is a useful metric as in many cases policy-makers want to rank locations by their relative ES values (Willcock and others 2016). The second metric was the average absolute deviance of modelled values from the 1-to-1 line representing a perfect fit of normalised model values to the normalised validation values—a measure of accuracy and trueness, as it reflects the degree to which models consistently reflect validation values (SI-2). In our normalised setting (with values inverted for consistency with ρ), deviance ranged from 0 (poor fit) to 1 (perfect fit). For interpretation, we follow the generally used criteria employed in AUC (area under the curve) in which a result below 0.7 should be considered as likely random (Swets and others 1979; Marmion and others 2009; Hooftman and others 2016) and a value of at least 0.7 shows a close fit between the modelled value and the validation data. It is entirely possible for a model to have a high rank correlation value, but also have high deviance from the 1–1 line and vice versa, so the two metrics are complementary (Table 2, Figure 3). We calculated both metrics separately for every ES model for each relevant validation dataset, with the ES models run at 1 × 1 km spatial resolution in most instances, giving 100 comparisons (carbon: 12; water supply: 21; water use: 18; charcoal use: 8; firewood use: 15; grazing use: 26 Figure 1).
The Effect of Model Complexity, Spatial Extent and Adding Beneficiaries on ES Model Performance
For each ES, we assessed model complexity in terms of the number of input variables (input complexity [IC]). We considered an input to include a coherent set of values covering a geographic region for a single feature (for example, land use or elevation). GIS processing without changing the feature parameter was not considered an additional input, and neither were layers created by combining inputs, although the parameter values of an equation could be independent, single-value datasets (see SI-4 for full details). Thus, our new models (developed via GIS processing of the outputs from the existing models of ES potential) retained the complexity score of the associated existing model (Figure 1; SI-4). As such, our complexity metric captures the generalisation that models with large numbers of equations generally require more inputs (Sun and others 2016). From a user experience perspective, this complexity often relates to the sourcing and processing of these required input datasets (Willcock and others 2016). Our continuous complexity metric is more subtle and precise than simple categorisation of models, for example, process-based vs production function. Therefore, it allowed us to advance from previous model comparisons, which often focus on identification of the best model specific to a location, by identifying generalisable conclusions relating model complexity to model accuracy. We log-transformed the IC value (LIC) in all instances as the data were skewed by extreme values.
Importantly, we considered each separate model vs validation dataset comparison a single independent data point (for example, InVEST stored carbon validated against carbon storage per unit area derived from tree inventory plots was a single data point) (Figure 1). This is because we were interested in assessing how well models performed in general in sub-Saharan Africa for different types of validation data collected in different locations. This approach also enabled us to use very different types of validation datasets, thereby overcoming the issue of there not being consistent validation data for all ES across most of sub-Saharan Africa.
By considering each model vs validation dataset comparison (in terms of rank correlation or deviance) a single data point, we were able to build separate generalised linear models (GLMs) for each of the two model performance measures (the response variable y; rank correlation or deviance), and for each ES. In each case, the GLM was: y ~ Complexity Measure + Spatial Extent. Thus, LIC was chosen as the complexity metric, with spatial extent (local, regional, country) modelled as a fixed factor. This allowed us to test if more complex models better predict the biophysical supply or realised use of each of ES, whilst controlling for any effects of spatial extent. Where the validation data were of realised ES, we compared models of potential ES, ES demand and realised ES.
In general, at least one model for each ES produced outputs that represented the validation data well, calculated in terms of their deviance measure and Spearman’s ρ, with deviance showing better fits (mean of the least squares mean [LSM] values for best-fit model: ρ = 0.43, deviance = 0.76; Table 2; Figure 3; SI-2). Potential ES: The LSM value of the response variable for the best-fit model showed that the best of the existing models of potential ES (carbon and water supply) matched the validation data well (mean LSM value for best-fit potential ES models: ρ = 0.69, deviance = 0.82; Table 2; Figure 3A). Realised ES: Whilst still producing reasonable fit to validation data, the new models of realised ES did not show a fit as good as the models of potential ES to their respective validation data (mean LSM value for best-fit realised ES models: ρ = 0.30, deviance = 0.73; Table 2; Figure 3B). When compared to realised ES data (Table 3), some (3 of 8 [38%]) of the simple models of realised ES performed better than models of ES potential, and none performed worse. However, for our models of realised charcoal, firewood and grazing services, a majority (45 of 47 [96%]) were predicted as well by human population density alone as by our models, and in two cases (4%) population density was a better predictor than our models (p values < 0.05; Table 2). By contrast, the comparison of realised water with the water use data showed population density to be a worse predictor than our new realised ES models (6 of 6 [100%]; Table 2).
Our comparisons showed either no (1 of 4 [25%] potential ES; 6 of 8 [75%] realised ES) or a positive (3 of 4 [75%] potential ES; 2 of 8 [25%] realised ES) effect of complexity on model fit, with no cases of a negative effect (Table 3). Responses to model complexity were not consistent among the two model accuracy metrics (ρ and deviance), reflecting their different properties. Notably, we found positive effects across both metrics for stored carbon, but complexity was more rarely a significant predictor of model fit for firewood use, charcoal use and water availability, and in these cases was only detected for one of the two accuracy metrics. Grazing use and water use showed no effect of complexity for either metric (Table 3).
This study—the first multi-country validation of multiple ES models (to the best of our knowledge)—suggests that the existing ES models provide good predictions across two potential ES of high policy relevance (Willcock and others 2016). But, for the ES models we investigated, models of potential ES (biophysical supply) were more accurate than our new models of realised ES (use; Table 2). This difference can be explained by the facts that: a) building models for realised ES is more challenging; and b) there is a research bias towards the biophysical supply of a few provisioning and regulating services—food supply, water availability and stored carbon (Egoh and others 2012; Martínez-Harms and Balvanera 2012; Wong and others 2014).
The Importance of Social Systems
Decision makers require information on a wide range of ES and across a variety of temporal and spatial scales (Scholes and others 2013; McKenzie and others 2014; Willcock and others 2016). Meeting these needs will require a shift in the focus of most models towards understanding the beneficiaries of ES and quantifying their demand, access to and utilisation of services, as well as the consequences for well-being (Bagstad and others 2014; Poppy and others 2014). Whilst some studies (Hamann and others 2016) and models (Mulligan 2015; Suwarno and others 2018; Martínez-López and others 2019) do include the demand and use of ES, our new models of realised ES (created by weighting outputs of models of ES potential by human population) generally showed lower predictive power when compared with the ability of the existing models of ES potential to predict biophysical supply. Indeed, many of our new models were unable to predict ES more accurately than human population density alone (Table 2, Table 3). This suggests that rural human population density is a good proxy for ES demand, and realised use of ES is closely aligned with demand in sub-Saharan Africa. The only exception is water use, where our new models were better predictors of realised water use than human population density (Table 2). Further combining social science theory and data to explain the social–ecological processes of ES co-production, use and well-being consequences will likely result in substantial improvements in our understanding and estimates of ES use (Bagstad and others 2014; Díaz and others 2015; Suich and others 2015; Pascual and others 2017). This is an area of active research, and some modelling frameworks are beginning to address this deficiency. Socio-economic data on ES use, perceptions and well-being contributions collected over large regions can and has been incorporated into models to address questions about the impacts of ecosystem change on the well-being of regional and socio-economic groups (Díaz and others 2015; Hamann and others 2016; Egarter Vigl and others 2017). Spatial multi-criteria analyses can be used to model how consistent available potential ES are with local demand, highlighting trade-offs between beneficiary groups where demand varies (Martínez-López and others 2019). Furthermore, the impact of individual decision-making on ES use can be captured through the integration of agent-based models depicting human behaviour with biophysical models (Villa and others 2017; Suwarno and others 2018)). Coupling models of potential ES with models of demand to estimate realised ES will likely result in models that are more complex than the existing models (Zhang and others 2017), which our findings suggest could improve accuracy, and new modelling techniques (for example, machine learning (Willcock and others 2018)) may be needed to enable this (Bryant and others 2018).
The Impact of Model Complexity
The effect of model complexity on the accuracy of ES results has not been investigated in detail previously. For example, a Web of Science search (20 June 2018) for ‘model’ and ‘complexity’ and ‘accuracy’ and ‘ecosystem service’ resulted in only 19 studies, few of which actually assess how ES model complexity affects accuracy. Our results suggested a tendency for ES model complexity to be correlated with increased performance (particularly for potential ES), and strong evidence that increased model complexity does not lead to worse predictions (for both potential and realised ES). However, each successive increase in complexity brings diminishing returns. For example, for each unit increase in LIC for models of stored carbon, ρ increased by 0.25 and deviance by 0.10 (Table 3). Since LIC is log-transformed, each unit increase is achieved by a tenfold increase in inputs. Furthermore, a trade-off with benefits of additional complexity may be the feasibility of running and interpreting such models (Willcock and others 2016). Results from elsewhere in the literature are mixed, often dependent on the specific context of the comparison. For example, Villarino and others (2014) compare simple ‘Tier 1’ carbon accounting methods with more complex ‘Tier 2’ methods, reporting increased accuracy with model complexity. However, studies that extend this analysis to the most complex ‘Tier 3’ methods report limits in the gains in accuracy, with intermediate ‘Tier 2’ and complex ‘Tier 3’ models producing similar predictions (Hill and others 2013; Willcock and others 2014). Furthermore, increasing model complexity does not necessarily lead to better model performance when predicting ground water recharge rates (von Freyberg and others 2015) nor agricultural yield (Quiroz and others 2017). Nevertheless, model performance should not be the only variable considered when selecting between models of differing complexity. From an ecological perspective, simple functional forms (for example, linear or nonlinear regression equations having a sufficiently high explanatory power) can be easier to interpret and translate into applications (that is, from science to policy). However, they may lack predictive power in novel locations and/or future time points if they insufficiently represent spatial heterogeneity in form and process (Syfert and others 2013). A certain level of complexity may be required before sufficiently reliable results can be obtained (Merow and others 2014; Salmina and others 2016), such as our observation that human population is poor predictor of water use, likely as it completely fails to capture the behaviour of the presence and flow of water. Simpler models may accurately represent more basic aspects of a system (for example, estimating natural capital), but incorporation of additional complexity may be necessary to describe the underlying processes accurately (for example, the interactions and feedbacks between people and ecosystems) (Merow and others 2014; Willcock and others 2014; Dunham and Grand 2016), and how different trade-offs and benefit flows can be understood and managed. Thus, model complexity should be considered in terms of how complex the ES being modelled are, what objectives need to be met, and to what end.
Our analysis comes with several important caveats with respect to validation. Here, we highlight these in part to act as a ‘call to arms’ for ES scientists concerning areas demanding further development.
Primary data collection, particularly at large scales, should be a priority for ES scientists. As validation of modelled outputs must involve like-for-like comparisons (that is, comparing potential ES outputs to biophysical supply and realised ES outputs to observed ES use), we were unable to validate all models and we would have liked. For example, we were unable to include the models of realised ES produced by Co$ting Nature (Mulligan and others 2010; Mulligan 2015) due to the lack of corresponding validation data.
Another priority for future work is to link better different types of ES models to bespoke validation data to understand their performance fully. For instance, the different carbon models we used to some extent model different constructs. Co$ting Nature’s stored carbon model includes both below- and above-ground carbon, whilst other models predict only above-ground carbon (see SI-1), and we validated these with above-ground carbon data. As below-ground carbon can exceed that of above ground, these data are not ideal to validate the Co$ting Nature model. As below-ground carbon in forests is often consistent across forests or proportional to above-ground carbon storage (Lewis and others 2013), it is unlikely that this particular issue affected our findings. However, similar issues arise when linking the Costanza and others (2014) benefit transfer models with validation data, as the former estimate value but are validated against either biophysical or use data (SI-1). Because benefit transfer models are derived by combining global values with land cover data, one might expect the values to be more indicative of the biophysical supply of services, but be poorly matched to actual ES use. To reduce these issues and enable like-for-like comparisons, we generated new models (for example, for firewood, charcoal and grazing resources) from stored carbon outputs of the existing models (SI-1) in our analyses. These new models used spatial masks to estimate the biomass available on relevant land uses (SI-1). The outputs from these new models are likely to be overestimates as, for example, not all grassland vegetation will be grazed and not all grazed land will stock at maximum capacity (Fetzel and others 2017). However, since our statistical analyses focused on relative ranking (see methods), it is unlikely that these uncertainties impacted our findings greatly (that is, sites with the highest maximum capacity are likely to be the sites with highest potential and/or realised grazing).
More generally, it may be good practice to validate models against more than one dataset, as validation data have their own intrinsic inaccuracies. For example, in this study we used more than one validation dataset for each ES (Table 1). More work is required to understand how best to validate ES models, allowing model validation to become standard practice within the ES community, increasing confidence and helping to reduce the implementation gap between ES models and policy- and decision-making (Cash and others 2003; Voinov and others 2014; Wong and others 2014; Clark and others 2016). However, there will always be financial and practical limits to model validation, especially at large scales. Collection of high-quality data is challenging and expensive, and as such would require further investments; indeed, the reason ES models are used is often because of the lack of primary data.
Finally, more work is required to develop and test more complex use models. Whilst we highlight that ES models need to move beyond biophysical production to realised use by beneficiaries, our very simple ES use models require substantial improvement, for example, by incorporating flows of ES (Bagstad and others 2014; Villa and others 2014). Similarly, none of the models we consider here adequately represent temporal dynamics (that is, when are ES being used?) (Scholes and others 2013; Willcock and others 2016), nor can they disaggregate between beneficiary groups (that is, who is using which services?) (García-Nieto and others 2013; Bagstad and others 2014), nor estimate if such use is sustainable. All three points are highly relevant to understanding if the Sustainable Development Goals (https://sustainabledevelopment.un.org/) are being achieved, and hence represent a critical and hugely challenging frontier in both ES modelling and validation. This is further complicated by the fact that model reliability may differ across spatial scales (Scholes and others 2013). For example, because the focus of decision-makers across sub-Saharan Africa predominantly ranges from local to national scales, they require ES information at different gridcell sizes (Willcock and others 2016), and so it is necessary to understand better how the accuracy of ES models varies with spatial resolution.
Our study demonstrates the feasibility of ES model validation, even in data-deficient locations such as sub-Saharan Africa (Suich and others 2015; Willcock and others 2016). Although this demonstration has been long overdue, the lack of such large-scale, multi-model validations is perhaps reflective of the complications involved. In partnership with decision-makers, the advances suggested here could help to ensure ES research continues to inform ongoing policy processes (Voinov and others 2014) (such as the IPBES, the Sustainable Development Goals and CBD Aichi targets). Our findings are of particular relevance to sub-Saharan Africa. Whilst the continent is perceived as relatively data-deficient (Suich and others 2015; Willcock and others 2016), we have shown that adequate data exist to run and validate multiple models for ES of high policy relevance (Willcock and others 2016), particularly related to supplies of ES. Thus, ES models could help to meet the information demand from policy-makers in sub-Saharan Africa (Willcock and others 2016).
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This work took place under the ‘WISER: Which Ecosystem Service Models Best Capture the Needs of the Rural Poor?’ project (NE/L001322/1), funded by the UK Ecosystem Services for Poverty Alleviation program (ESPA; www.espa.ac.uk). ESPA receives its funding from the UK Department for International Development, the Economic and Social Research Council and the Natural Environment Research Council. We thank Kate Schreckenberg and the anonymous reviewers, whose input substantially improved the manuscript.
Conflict of interest
The authors declare that they have no conflict of interest.
FE, SW, DAPH, TPD, POF, MDH, BR, CS, FV and JMB conceived the project. SW, DAPH, RB, TPD, POF, MDH, MM, BR, CS, NS, FV, FE and JMB developed the investigation at a workshop on model complexity. SW and SMW collated and prepared the validation dataset. SW and MM ran the Co$ting Nature and WaterWorld models. DAPH ran the InVEST models and Scholes international and water supply models. SW, SB and JML ran LPJ-GUESS, ML provided the LPJ-GUESS code and, with TH, provided advice on the use of LPJ-GUESS. RB, POF and BR ran the local South African grazing and firewood models. DAPH, JMB, SW and FE analysed the results. SW, DAPH, FE and JMB wrote the manuscript, with comments and revisions from all other authors. DAPH collated the SI, with comments and revisions from all other authors.
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Willcock, S., Hooftman, D.A.P., Balbi, S. et al. A Continental-Scale Validation of Ecosystem Service Models. Ecosystems 22, 1902–1917 (2019). https://doi.org/10.1007/s10021-019-00380-y
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