1. Introduction
Fire has always been a natural disturbance affecting and shaping Mediterranean-like landscapes, such as those in California, Australia, and southern Europe [
1,
2]. Amongst the southern European countries, Portugal is one of the most affected by wildfires, with an average burned area of almost 140,000 ha per year between 2010 and 2019 [
3].
In recent decades, fire has acquired different characteristics in response to changes in climate, but mostly due to a decline in the landscape mosaic that has historically characterized Portuguese rural areas [
4,
5,
6,
7]. The abandonment of agricultural activities in mountainous areas, previously linked to active management of fuel in the landscape, was accompanied by a landscape homogenization through shrub encroachment and afforestation with monocultures of non-native species (eucalyptus and maritime pine), causing a change in fire patterns, from frequent and low intensity to less frequent but more intense and extensive [
8]. At the same time, the increase in fire suppression efficiency also encouraged the continuous accumulation of fuel in the landscape, creating even more intense and extensive fires [
2]. These changes challenge policymakers and land use planners to develop effective policies to decrease the proportion of burned area in the landscape.
Wildfire susceptibility was recently reassessed [
9,
10], and the necessity of a landscape redesign to reduce the burned area has already been recognized by the Portuguese Government with the creation of the Landscape Transformation Program [
11]. However, information on how and where to transform the landscape to achieve this goal is still scarce.
Land systems (LSs), the classification of different land use and land cover (LULC) based on factors such as vegetation type, land management practices, and socio-economic activities, can have a significant influence on the occurrence, behavior, and impact of fires [
12,
13,
14]. In Portugal, fire-proneness decreases from shrubland areas to forests, with variations in species, to agricultural areas (annual and permanent crops, pastures, and agroforestry systems) and urban areas [
15,
16,
17,
18]. Livestock composition can have a dual effect on the burned area [
8]. While grazing goats, for example, are often associated with burning for pasture renewal, cattle and sheep tend to be associated with a reduction in the fine fuel load in the landscape [
19]. Holdings size constraint management actions [
20], associated with the fact that the property is mostly private, can restrict the implementation of landscape-level plans [
21]. Higher population densities are linked to higher fire ignitions but also to a higher early detection and effective firefighting; therefore, the extent of fires can be limited [
4]. These are important gradients to consider when the aim is to decrease the proportion of burned area with single altering LULC since it is the only variable influencing fire behavior that can be modified at the landscape scale [
7,
15].
Fire behavior is also directly influenced by land morphology (LM) [
22,
23,
24,
25,
26] since it promotes radiant energy transfer from low to higher topographical levels [
27]. Several studies report that topographic characteristics are the most significant variables affecting burn severity [
28,
29]. In mainland Portugal, between 1990 and 2017, around 46% of the burned area occurred on hillslopes with a slope greater than 16%, while the flattened areas (valleys bottoms and hilltops) only accounted for about 13%.
In addition to individual effects, other studies [
22,
23] have explored the relationships between LULC and topography in explaining fire behavior. Despite reaching partial contradictory results, both studies concluded that the proportion of burned area was not independent of slope for any LULC category. Still, how the interaction between LSs and LM affects fire behavior remains poorly understood.
Simultaneously, the spatial distribution of LS is conditioned by LM, leading to the generalization that flatter areas are more suitable for agriculture, while more sloping areas have greater suitability for forests and shrubs [
30,
31,
32,
33,
34,
35,
36]. Effectively, the difficult access for farming operations on larger slopes, and the consequent increase in the risk of erosion by agriculture, make forest and shrubland the more suitable LULC for these locations [
37], but at the cost of greatly increasing the proportion of the burned area.
The main objectives of this study are (i) to investigate differences in fire-proneness across LM and LS types at a national scale; (ii) to analyze the interaction effects between LM and LSs on burned area; and (iii) given the constraints that LM places on the distribution of LSs, identify whether there is scope to transform fire-prone landscapes by modifying LS.
To achieve these objectives, two typologies were created. A LM typology, based on three main landforms: valley bottoms, hillslopes, and hilltops. A LS typology, based on five key dimensions: land use, agricultural management intensity, livestock composition, land ownership structure, and demography. With the identification of homogeneous areas of fire-proneness, this study aims to establish priority areas for landscape transformation actions and the application of common strategies of landscape planning and management.
2. Materials and Methods
The study area is mainland Portugal, the most southwestern country on the European continent (
Figure 1). With an approximate area of 89,084 km
2, Portugal is bordered by the Atlantic Ocean to the West and south and by Spain to the north and east.
The biophysical environment varies greatly between the areas located north and south of the Tagus River. This variation is largely explained by the marked differences in relief, as most mountainous areas are located in the north (the highest peak is at 1993 m), where total precipitation is close to 2000 mm, and the average annual temperature varies between 6 °C and 15 °C. Except for some mountainous areas in the extreme south, the landscape south of the Tagus River is characterized by a gently waved relief, where the average altitude is around 250 m. In this region, precipitation decreases to approximately 500 mm, and the average annual temperature rises to about 17 °C. During the summer months, the relative humidity is below 70% throughout the mainland territory, dropping below 60% in the hotter inland regions.
Despite this climatic variability between the north and south, Portugal presents typical characteristics of a Mediterranean climate, with the highest temperatures, lowest relative humidity levels, and strongest winds concentrated in the summer period, namely, in July, August, and September, creating the optimal conditions for fire occurrence.
In 2015, agricultural areas (temporary crops, permanent crops, and permanent pastures) accounted for 31% of Portugal [
38] (
Table 1). If we combine the agroforestry systems, it is obvious that agricultural uses predominate south of the Tagus River. In Portugal, the main agroforestry system is called
montado, and it is characterized by low tree densities combined with agriculture and/or pastoral activities. The Portuguese
montado is mainly constituted by two native species: cork oak (
Quercus suber L.) and holm oak (
Quercus rotundifolia Lam.), in some areas in combination with stone pine (
Pinus pinea L.). The maintenance of the
montado has largely depended on support from the Common Agricultural Policy (CAP), with a focus on direct support for extensive livestock, with positive effects in terms of its low fire-proneness.
Forests and shrubland occupy a large extent of the country (nearly 40% and 15%, respectively) and predominate in the region north of the Tagus River (
Table 1). The predominant forest species are non-native maritime pine (
Pinus pinaster Aiton) (19% of the country) and eucalyptus (Eucalyptus spp.) (13% of the country). The forests of native species such as oaks (e.g.,
Quercus robur L.,
Q. pyrenaica Willd,
Q. faginea Lam.) are mainly located in less productive areas and/or in steep slopes.
Urban areas account for about 5% of the country, occupying 7% of the area north of the Tagus River and 3% of the south (
Figure A2). While the main cities are located along the coast, smaller settlements are dispersed across rural areas, often surrounded by forests and shrublands, and under a high fire-risk.
Most of the land is privately owned and the largest holdings prevail south of the Tagus River, which allowed the scale necessary for the economic viability of agroforestry systems. The northern region, particularly in the interior, is characterized by small holdings, which traditionally supported subsistence agriculture and are currently being abandoned and occupied by shrubs or subject to forest management.
2.1. Land Morphology
Land morphology (LM) is a classification of landforms according to their hydrological position in the watershed and typifies two systems in the hillslope profile: wet (concave) and dry (convex) [
36]. The wet system consists of streams, water bodies, and valley bottoms, including floodplains, defined as flat or concave areas adjacent to streams with a slope <5%. The dry system encompasses convex slope areas, commonly found on the upper parts of the hillslope profiles. It includes hilltops as convex areas with slopes <5%. The narrower forms correspond to ridgelines and the wider to large hilltops, commonly referred to as plateaus. Hillslopes were classified according to different slopes: 0–12%; 12–16%; 16–25%; and >25%.
The LM map with 25 m spatial resolution, based on flat areas, surface curvature, and hydrological features, was adapted from [
36].
2.2. Land Systems
We characterized land systems (LSs) from a list of variables at the parish level (the smallest administrative region in Portugal), whose relationship with fire has already been studied [
15,
22,
39,
40,
41,
42]. In this study, we considered that Portugal was administratively divided into 4050 parishes, with a variation in the area between 5.15 and 43,527.44 ha (mean = 2199.61 ha). Currently, the number of parishes is lower, as many smaller parishes have been aggregated.
We compiled the exploratory variables from LULC digital map from 2015 [
38], the 2009 Agricultural Census [
43], and the 2011 Census of Population and Housing [
44]. We further organized these variables into five dimensions (
Table 2): “Land use”, “Agricultural management intensity”, “Livestock composition”, “Land ownership structure”, and “Demography”. We also mapped each variable to understand its spatial distribution in the study area (
Figure A1,
Figure A2 and
Figure A3).
The “Land use” dimension was organized into three major classes: “Urban areas”, “Farmland”, and “Forest and shrubland”. “Farmland” is composed of agriculture (sum of temporary crops, permanent crops, and permanent pastures) and agroforestry systems. “Forest and shrubland” class is composed of forests, separated by species: cork oak (Quercus suber L.), holm oak (Quercus rotundifolia Lam.), other oaks and hardwood (e.g., Quercus robur L., Q. pyrenaica Willd, Q. faginea Lam.), chestnut (Castanea sativa L.), eucalyptus (Eucalyptus spp.), maritime pine (Pinus pinaster Aiton) and other softwood, stone pine (Pinus pinea L.), and shrubs and herbaceous vegetation. It is important to emphasize that in the elaboration of the LULC cartography from 2015, burned areas were classified according to the land use that existed before the fire.
The “Agricultural management intensity” is composed of the agricultural holding’s productivity (average standard output (EUR) per hectare of total land) and the grazing intensity, i.e., the livestock density. The “Livestock composition” dimension characterizes the presence of livestock by category (e.g., sheep, goats).
The “Land ownership structure” dimension corresponds to the average size of agricultural holdings, calculated by dividing the total number of holdings by the utilized agricultural area (UAA), i.e., by the total area taken up by arable land, permanent grassland, permanent crops, and kitchen gardens used by the holding, regardless of the type of tenure or of whether it is used as a part of common land.
In this study, the “Demography” dimension, whose indicator is “population density”, intends to represent the potential for land management. In Portugal, the highest population densities are associated with the largest cities, where there are greater proportions of people of working age, younger, and educated people. On the contrary, less populated parishes have a higher proportion of elderly people and less educated people [
45].
2.3. Fire Data
The fire database was assembled using the Portuguese Institute for Nature Conservation and Forests (ICNF) data. These data include the total burned area, date of occurrence, and its location for the selected period 1990–2017 in the 4050 parishes of Portugal (currently, this number is lower because some parishes were aggregated). For each parish, we estimated the accumulated burned area (ABA), i.e., the sum of all the areas that burned during the period 1990–2017. This was then expressed as the proportion of the parish area (
Figure 2) and used as an indicator of fire proneness. As the size of parishes varies significantly from the north to south of the country, this method reduces possible biases. The highest values of ABA are in the central and northern regions and the extreme south of Portugal.
2.4. Statistical Analysis
Land morphology (LM) and land system (LS) typologies were constructed using two unsupervised classification methods using parishes as units of analysis: principal component analysis (PCA) and Ward’s hierarchical clustering method (HCA).
The PCA, performed on a correlation matrix, was used to reduce data dimensionality from the LM and LS variables, involving eigenvalue calculation, and selection of principal components based on explained variance. A Varimax orthogonal rotation was applied to minimize the number of variables with high scores. Only factors with eigenvalues greater than 1 were considered in the HCA [
47].
The HCA was subsequently applied to cluster the data, with Ward’s method serving as the linkage criterion, aiming to minimize the variance within clusters and produce clusters of roughly equal sizes. The clustering results were further evaluated based on the resulting HCA dendrograms and using the “Elbow method”, i.e., using a plot of the sum of squared errors (SSE) versus the number of clusters. In clustering contexts, SSE refers to the sum of squared differences between each data point and the centroid of the cluster where the data point belongs. The optimal number of clusters to describe the structure in the dataset was determined by locating a breaking slope (“elbow point”) on the plot of the SSE versus the number of clusters. Subsequently, to better understand the results, we mapped the LM and LS types (clusters) using a geographic information system (GIS).
The LM types and LS types were cross-tabulated (contingency table), and a chi-square test was carried out to determine the statistical significance of the relationship between the two classifications.
We used the Shapiro–Wilk test to test data for normality, but this condition was not met. For this reason, we performed the Kruskal–Wallis rank-based nonparametric test and post hoc Dunn’s test to determine differences among the fire-proneness (ABA) of both LM types and LS types (significant values p ≤ 0.05). The adjustments to the p-value on Dunn’s test were realized with the “Bonferroni” method. We used boxplots to visualize the graphical result.
We also performed a two-way ANOVA to explore whether there was an interaction between the two independent variables (LM types and LS types) on the dependent variable (ABA). Although the analysis of variance (ANOVA) assumes that the data fit the normal distribution, it is not very sensitive to moderate deviations from normality. Several studies, using a variety of non-normal distributions, have shown that the false positive rate is not substantially affected by this violation of the assumption when the samples are large [
48,
49,
50].
We mapped the various combinations between LM and LS types and their effect on ABA using a GIS to visualize its spatial distribution.
Statistical analyses were carried out with R version 3.5.1 [
51], using the following packages: “psych” [
52], “nFactors” [
53], “FSA” [
54], “dunn.test” [
55], “rcompanion” [
56]. ArcGIS 10.6 software [
57] was used for mapping.
4. Discussion
The climate of Mediterranean regions, characterized by warm–dry summers and cold–humid winters, provides optimal conditions for the rapid growth of vegetation and the existence of frequent and intense fire events. The mountain landscapes of southern European countries such as Greece and Portugal have been subject to recent phenomena of agricultural abandonment and subsequent shrub encroachment and afforestation with monocultural forests of maritime pine and eucalyptus [
58,
59]. In addition to changes in land use, other LS dimensions influence the overall fire-proneness of the landscape, such as the average size of holdings, which is smaller in southern European countries than in the other mentioned regions and highly influence the ability to redesign the landscape to reduce the burned area.
The fire-proneness analysis of the various LS types revealed significant differences in line with other studies [
15,
17,
22,
23]. The LS types characterized by high proportions of shrubland and forest show greater fire-proneness when compared with LS types characterized by higher proportions of agricultural uses (temporary crops, permanent crops, permanent pastures, and agroforestry systems) and urban areas in the landscape [
7]. This gradient may be due to the lower amount of fuel that characterizes agricultural areas and urban areas concerning forests and shrubland. Furthermore, areas with higher proportions of urban areas have higher population densities and, thus, faster detection of ignitions, which, combined with better fighting capacities, enables early fire suppression [
19].
Although the land use information [
38] used to establish LS types that support fire proneness comparisons corresponds to a temporal snapshot (2015), the fact that the areas that burned just before that moment were classified with the LULC that existed before the fire occurrence (e.g., forest or other, instead of post-fire shrubland) has avoided establishing an erroneous causality between fire historical data (1990–2017) and the LULC (e.g., identifying shrubland as the cause when they would be the consequence of fire).
Fire behavior is also influenced by land morphology (LM). The LM types “Hilly” and “Steep”, characterized by high proportions of steep sloping areas, have the highest rate of fire spread [
27]. Notwithstanding, LM types induce changes in the LS types’ fire-proneness, which generally increases with the increase in the proportion of steep slopes in the landscape.
From the classification of eight LS types, three stand out for their greater fire proneness: “MpiShr”, “ShrOak”, and ”Eucalyp”. The LS type “MpiShr” (maritime pine forests and shrubland grazed by goats) reveals the highest fire-proneness, which may be due to the composition of maritime pine (
Pinus pinaster Aiton) and shrubland, both LULC of high fire-proneness [
15,
22,
60], combined with a predominant distribution in the LM type “Steep” [
22,
23].
The LS type “ShrOak” (shrubland and other oaks and hardwood forests) also has a high fire-proneness. This type is mostly characterized by areas of natural succession in several stages, where extensive shrubland areas are punctuated by small oak forests, many of them non-mature. Despite the high fire-proneness of this type, the increase in agricultural areas and oak forests and the decrease in maritime pine forests compared with the LS type “MpiShr” negatively affect the burned area. This result is in line with a study that suggests that oak woodlands are generally more fire-resistant than coniferous forests and that an increase in their proportion may result in a decrease in the landscape’s susceptibility to fire [
6]. Still, under these circumstances, where small oak forests are located in extensive fire-prone areas of shrubland, it is possible that their fire resistance potential is being reduced. Moreover, shrubland is linked to the control of the extension of burned areas in the landscape [
60]. Usually, shrublands have the highest number of ignitions (e.g., burning for pastures) [
22] and, simultaneously, are considered the least valuable land cover and are given the lowest priority for firefighting. It should be noted that there are variations in the composition of shrubland areas that are not mapped and that will certainly have an impact on fire-proneness. Still, shrublands are essential for biodiversity conservation and the provision of several ecosystem services (e.g., soil protection) [
61], and its full elimination is not desirable, but rather its integration into a landscape mosaic. Several studies emphasize the importance of preserving a landscape mosaic to decrease the proportion of burned area in the landscape [
1,
5,
58,
62].
The LS type “Eucalyp”, characterized by the highest proportion of eucalyptus forests of all LS types, also has high fire-proneness. This may be related to the fact that this LS type is mostly located in the LM type “Steep”, with the high flammability of
Eucalyptus spp. [
63], and also because of the large extent occupied by this species in the landscape.
The association between LM types and LS types determines the distribution of LS in the landscape. In general, there is a predominance of LS types with greater proportions of forest (forests and shrubland) in the LM type “Steep” and of LS types with greater proportions of farmland and urban areas in the LM types “Gently wavy” and “Hilly”. The constraints placed by LM on LS could suggest that there was little room to transform the landscape to decrease the proportion of burned area, using a single strategy of increasing agricultural proportion. However, our results show that there are LS types of agricultural character of low fire-proneness (e.g., “MedAgr”, “ShpAgr”) located in LM types with high fire-proneness (e.g., “Steep”). Indeed, LS types linked with livestock grazing [
35,
64,
65] or permanent crops (e.g., vineyards, olive trees), often with terracing practice to prevent soil erosion and facilitate farming operations, are historically adapted to steep areas [
66,
67].
Despite LM’s influence on LS fire-proneness, LS types reveal an even greater effect on the proportion of burned area when we control for the effect of LM. For example, by changing the LS type from “MpiShr” (LS type with highest fire-proneness) to “IntAgr” in the LM type “Steep” (LM type with the highest fire-proneness), the proportion of the burned area is reduced to about one fifth. A landscape transformation at this level, where forests and natural habitats would be replaced with intensive farming systems, could be reflected in a large decrease in the proportion of burned area and an increase of agricultural commodity production, but probably at the expense of a broad range of services, including cultural heritage and identity [
68,
69], and the loss of biodiversity [
70]. In Europe, around 50% of all species rely on agricultural habitats at least to some extent [
71], so supporting specific types of low-intensity agriculture would potentially contribute to biodiversity conservation [
72]. When located on the wildland–urban interface, the maintenance of low-intensity agricultural areas in steep areas is also essential for the protection of settlements from fire [
73].
In general, the proportion of burned area in the landscape decreases as the proportion of agricultural uses increases, suggesting that it is a priority to balance the proportion between forestry (forests and shrubland) and agricultural uses in the landscape, to the detriment of other actions that aim to reduce landscape-scale fire-proneness. Our findings suggest that a proportion of more than 40% of agricultural uses in the landscape (e.g., LS Type “MedAgr”, “ShpAgr”, “LgScAgr”) results in a reduction of about 50% in the burned area in the LM type with the highest fire-proneness (“Steep”) (
Table 4), compared with landscapes where agriculture only occupies less than 26% (e.g., LS types “MpiShr”, “ShrOak”, and “Eucalyp”).
The LS types are also influenced by the land ownership structure, namely by the size of the holdings [
74]. For example, in the LS type “LgScAgr”, characterized by the largest average size of holdings, it was possible for farmers to run economically viable agroforestry systems (in Portugal, mainly associated with cork oak and holm oak agroforestry systems). This LS type, which also has a high proportion of cork oak and holm oak forests outside agroforestry systems, reveals a low fire-proneness, particularly when compared with the LS type “ShrOak”, where small oak forests are associated with extensive areas of shrubland in small-scale farm areas. Of course, it cannot be ignored that this agro-forest-based LS type predominates in the LM types “Gently wavy” and “Hilly”, where there are fewer restrictions on the implementation and management of fuel within the farming systems. It is also worth noting that the LS type “LgScAgr” has the second lowest population density of the eight types and the second lowest fire-proneness, alongside the LS type “IntAgr”, revealing that it is possible to create less fire-susceptible landscapes, even in areas with low population density.
To achieve landscapes with lower proportions of burned area, transformation actions should prioritize LM types characterized by large proportions of steep slopes and LS composed of high proportions of shrubland and forests. Here, efforts must be made to increase the proportion of agricultural area, using innovative policy-support solutions and sustainable agricultural practices to make this activity economically viable and, at the same time, avoid negative impacts greater than the fire itself (e.g., soil erosion).
The Landscape Transformation Program [
11] identified the territories with the highest fire risk and encouraged the joint action of farmers and forest owners to create a landscape mosaic in these territories, against the payment for ecosystem services. For these actions to be possible, it is necessary to mobilize a substantial part of the Common Agricultural Policy (CAP) funds for these fire-prone areas.
However, in Portugal, as a significant part of CAP support is given depending on the extent of agricultural holdings [
75], the large holdings in the South receive most of the funding, with positive results regarding the decrease in the burned area. When distributed based on the extent of the holdings, CAP support fails to consider, e.g., the employment, production or the provisioning of ecosystem services. For the CAP to contribute to reducing the proportion of burned area in the more fire-prone landscapes, it is necessary to partly allocate financial support to the small farms in the less-favored and steep areas, based, e.g., on the provisioning of ecosystem services such as fire protection [
76].
Increasing the proportion of agriculture in the landscape can be difficult to achieve at a large scale in the short- to medium-term, or not desirable in some situations (e.g., low suitability areas; nature conservation areas), so parallel actions can be taken to decrease the proportion of burned area in the landscape. As relevant alternatives, we highlight the gradual change in the composition of forests to low-flammability native species, spatially distributed according to the ecological suitability of the land [
77] or rewilding initiatives, where unplanned fires under favorable weather conditions, can create new open areas, contributing to biodiversity and increasing fire suppression opportunities at the landscape level [
78].
5. Conclusions
Fire behavior is influenced by land systems (LSs), and there is a decreasing gradient of fire-proneness from LSs characterized by a higher proportion of shrubland and forests, to those with higher proportions of agriculture and urban areas. Even so, there are differences in fire-proneness regarding the composition of forest and agricultural spaces. In turn, the LS distribution is influenced by land morphology (LM) which, in parallel, also influences fire behavior, with landscapes composed of higher proportions of steep slopes revealing greater fire-proneness.
Although LM constrains the spatial distribution of LS, with more fire-prone LS dominating in steeper regions, there are less fire-prone LS adapted to these morphological conditions (e.g., Mediterranean agriculture, grazing sheep).
The use of typologies allowed the identification of homogeneous areas of LM and LS for the application of common strategies of landscape planning and management. Actions to transform the landscape must prioritize regions characterized by high proportions of steep slopes, whose dominant composition is forest and shrubland. A balance between forest and agricultural uses must be encouraged to achieve a fire-resilient landscape. The results of this study suggest that a proportion of about 40% of agricultural uses (temporary crops, permanent crops, permanent pastures, and agroforestry systems) in the landscape results in a reduction of about 50% in the burned area, compared with landscapes where agriculture only occupies less than 25%.
The European Union’s Common Agricultural Policy (CAP) is a financing instrument that addresses natural hazards, including fire, and its funds can contribute to promoting the development of agriculture (e.g., Mediterranean agriculture, grazing) in areas with greater fire-proneness, also focusing on the wildland–urban interface, recovering the traditional agricultural belt around the villages.