Flood Hazard Assessment Mapping in Burned and Urban Areas

: This study proposes a simple method to produce a ﬂood hazard assessment map in burned and urban areas, where primary data are scarce. The study area is a municipal unit of Nea Makri, a coastal part of the eastern Attica peninsula (central Greece), which has been strongly urbanized and suffered damage from urban ﬁres in 2018. Six factors were considered as the parameters most controlling runoff when it overdraws the drainage system’s capacity. The analytical hierarchy process (AHP) method and a geographical information system (GIS) were utilized to create the ﬂood hazard assessment map. The outcome revealed that the areas with highest ﬂood hazard are distributed in the eastern and southern parts of the study area, as a result of the combination of lowlands with gentle slopes, torrential behavior of the streams, streams covered by construction, increasing urbanization and burned areas. The uncertainty and the veriﬁcation analyses demonstrate a robust behavior for the model predictions, as well as reliability and accuracy of the map. Comparing the existing urban fabric and road network to the potential ﬂood hazard areas showed that 80% of the urban areas and 50% of the road network were situated within areas prone to ﬂood. The method may be applied to land use planning projects, ﬂood hazard mitigation and post-ﬁre management.


Introduction
The Earth landscape is a result of the interaction of several parameters, such as the geomorphic process, climate and human activity. Natural hazards are physical events, able to influence the natural and human environment significantly. In this context, the morphological changes of landforms due to natural disasters can restrict human interaction with the ecosystem [1][2][3][4][5][6][7][8][9][10][11][12].
Floods have affected the natural environment, before humans' appearance on Earth. Nowadays, they are considered natural hazards and a significant global problem threatening human life [13,14].
Floods have a significant impact on the development of a region. Historically, floods have large consequences for individuals and communities which include loss of human life, damage to buildings and infrastructure, destruction of crops, disruption to social affairs and loss of livestock [15,16].
In Europe, floods are among the most expensive types of natural disasters with costs about €4 billion per year over the period 2000-2020. Flooding is less significant in inner continental countries compared to Mediterranean countries [17].
On the other hand, floods after a fire are typically more extensive than before wildfires. Worldwide, fires burn more than 300 Mha h −1 per year, and in the Euro-Mediterranean region, wildfires burn about 450,000 ha per year [18][19][20]. Greece in particular experienced unusually high burned areas in 2007 and 2018. In the aftermath of wildfires, all surrounding and impacted areas are at risk of flooding for several years. Damaged areas are left without

Materials and Methods
The case study area is the municipal unit of Nea Makri and is a popular holiday resort. It is located on the coast of Marathon Bay, a bay of the South Euboean Gulf, in the northeastern part of Attica Prefecture ( Figure 1A). It is bounded on its western-southwestern part by Mount Pentelikon, while the hill Agriliki dominates its northern part. The area is a popular tourist destination with holiday houses, hotels and yacht marinas.
The study area occupies approximately 34 km 2 , and it is a low altitude area, with elevation varying from 0 to 782 m above sea level. Gentle slopes characterize its morphology, while only the western and northwestern parts of the basin are mountainous ( Figure 1B).
As regards climatic conditions, the study area has a Mediterranean climate type. The mean annual temperature reaches 18 • C and the yearly precipitation is 400 mm.
Several streams drain the study area. They have a limited length and their drainage basins have small areas. The length of their mainstream channel varies from 0.2 to 5.5 km. The steams debouch northeastwards from the eastern flank of Mount Pentelikon to the South Euboean Gulf ( Figure 1B). Their flow is ephemeral, and they have torrential behavior. Although such fluvial systems in semiarid areas are frequently dry, extreme flash floods happen.
The study area was severely hit by fire on 23 July 2018. The fire started on the Pentelikon Mountain, spread very quickly to the seaside towns of Mati and Neos Voutzas ( Figure 1B) and grew into one of the largest urban wildfires in recent European history, which left 102 people dead and 164 injured. Seventy percent of Mati was utterly burnt from the wildfires, while the remaining 30% was either partially burned or contains burnt areas. Houses and vehicles were totally burned, leaving Mati and nearby towns completely destroyed [38,39]. As regards climatic conditions, the study area has a Mediterranean climate type. The mean annual temperature reaches 18 °C and the yearly precipitation is 400 mm.
Several streams drain the study area. They have a limited length and their drainage basins have small areas. The length of their mainstream channel varies from 0.2 to 5.5 km. The steams debouch northeastwards from the eastern flank of Mount Pentelikon to the South Euboean Gulf ( Figure 1B). Their flow is ephemeral, and they have torrential behavior. Although such fluvial systems in semiarid areas are frequently dry, extreme flash floods happen.
The study area was severely hit by fire on 23 July 2018. The fire started on the Pentelikon Mountain, spread very quickly to the seaside towns of Mati and Neos Voutzas ( Figure 1B) and grew into one of the largest urban wildfires in recent European history, which left 102 people dead and 164 injured. Seventy percent of Mati was utterly burnt from the wildfires, while the remaining 30% was either partially burned or contains burnt areas. Houses and vehicles were totally burned, leaving Mati and nearby towns completely destroyed [38,39].
Since the early 21st century, the region has strongly urbanized and its population has greatly increased [40]. Unchecked constructions block parts of the drainage network. The lowland areas of the towns Nea Makri, Zouberi and Mati have repeatedly been affected by flood events during extreme storm events [41].

Data
The used data and their sources in the present work were:  Since the early 21st century, the region has strongly urbanized and its population has greatly increased [40]. Unchecked constructions block parts of the drainage network. The lowland areas of the towns Nea Makri, Zouberi and Mati have repeatedly been affected by flood events during extreme storm events [41].

Data
The used data and their sources in the present work were:

Applied Method
Flood hazard mapping can be achieved by using hydraulic-hydrodynamic methods. An advantage of these models is that the indicated hazard maps are usually connected to certain return periods according to the European flood directive, even though they need data which are often not able to be obtained at a scale of the drainage basin [26][27][28][29][30][31][32]44,45].
In the present study, the lack of data related to precipitation and especially discharge gauges resulted in limitations to the hydrologic analysis. Thus, the link of the flood hazard assessment to return periods was not feasible. Otherwise, the AHP method was applied to produce the flood hazard assessment model. The method has been commonly used to delineate flood-prone areas since this approach warrants accurate and reliable predictions. For instance, Rahmati, et al. [27] used the AHP to map the flood-susceptible areas in Yasooj region, Iran, while Fernández and Lutz [28] applied the same method to assess flood hazard zoning in Tucumán Province, Argentina. In Greece, several researchers used the AHP method to assess potential flood-prone areas; i.e., Stefanidis and Stathis [29] in Kassandra Peninsula (northern Greece), Papaioannou et al. [45] in Thessaly (central Greece), Bathellos et al. [46] in northeastern Peloponnesus (southern Greece) and Skilodimou et al. [47] in the drainage basin of Pinios River (western Greece). Additionally, Bathrellos et al. [32] applied this method to produce an urban flood hazard map in the metropolitan urban area of Athens, capital of Greece.
Saaty [33][34][35] proposed the AHP method, which implements a linear correlation between the factors involved. The application of the method in flood hazard assessment, including the pair-wise comparison, the creation of the table-matrix, the calculating of the weighting coefficients, as well as the computation of the consistency ratio, was analyzed in detail in the published work [32].

Involved Factors
The applied model is based on the factors which control the route of water when the capacity of the drainage network is exceeded by an extreme flood event. Previous published works [12,13,26,27,32,[45][46][47][48][49] as well as data availability were utilized for the selection of the appropriate factors. Six physical and anthropogenic factors were taken into account. The physical factors were slope, elevation, distance from open channel streams, and hydrolithology, while the anthropogenic factors were distance from totally covered streams, along with land cover.

Slope
Since steep slopes contribute to flood occurrences and gentle slopes are more susceptible to flooding, slope is an essential factor for flood hazard assessment. Since a high-resolution digital terrain model (DEM) of the study area was not available, contours (4 m interval) and elevation points of the topographic diagrams were used to produce a DEM. The data were interpolated by using the topo to raster method, which is based on the ANUDEM program developed by Hutchinson [50]. Although DEMs derived from contour lines and elevation points often have bias, this method has a minor bias in the interpolation algorithm that may result in misleading results when calculating the profile curvature of the output surface, but is otherwise not noticeable [50]. According to Arun [51], the ANUDEM interpolation method is preferable for streams and adapted itself to terrain variations. Therefore, this method was considered to be the most appropriate to meet the requirements of the present work. The DEM was used to create the slope layer which was separated into five classes (Figure 2A

Distance from Open Channel Streams
Streams are a significant parameter for flood hazard assessment. The drainage networks were obtained from the topographic maps (scale 1:5000) and were digitized as a line layer. The Strahler's stream order system was used to define the streams. Third and higher order streams were studied, as they can cause flood events. The drainage networks

Elevation
Lowlands are flood-prone areas, and thus elevation is a vital factor in flood hazard estimation. As in the case of slope, the DEM was used to create the elevation layer. It was classified into the following, i.e., (i) <50 m a.s.l., (ii) 50-100 m a.s.l., (iii) 100-200 m a.s.l., (iv) 200-300 m a.s.l. and (v) >300 m a.s.l. ( Figure 2B).

Distance from Open Channel Streams
Streams are a significant parameter for flood hazard assessment. The drainage networks were obtained from the topographic maps (scale 1:5000) and were digitized as a line layer. The Strahler's stream order system was used to define the streams. Third and higher order streams were studied, as they can cause flood events. The drainage networks of the study area consist of open channel streams and streams covered by urban fabric (Figure 3). The open channel streams were mapped through extensive fieldwork.

Hydrolithology
The geologic conditions influence the surface runoff and may also contribute to flooding occurrences and flood hazard. The geological formations derived from the geological map of the study area were categorized into three classes according to their hydrolithological status [52]. They are (i) permeable, (ii) semi-permeable and (iii) impermeable formations ( Figure 4A). Buffer zones were created around third-order streams at distances of 50, 100, 200 and 300 m ( Figure 3A), and fourth-order streams at distances of 100, 200, 300 and 400 m ( Figure 3C).

Distance from Totally Covered Streams
As in the case of open channel streams, the totally covered streams were identified and mapped in detail through extensive fieldwork. Buffer zones were generated around the totally covered streams of the study area, i.e., third-order streams at distances of 50, 100, 200 and 400 m ( Figure 3B) and fourth-order streams at distances of 100, 200, 300 and 500 m ( Figure 3D).

Hydrolithology
The geologic conditions influence the surface runoff and may also contribute to flooding occurrences and flood hazard. The geological formations derived from the geological map of the study area were categorized into three classes according to their hydrolithological status [52]. They are (i) permeable, (ii) semi-permeable and (iii) impermeable formations ( Figure 4A).

Land Cover
Since the vegetation can help absorb rainfall, land cover influences the occurrence of floods. Since high-resolution land use data of the study area were not available, the land cover of the study area was taken from the CORINE 2012 Land Cover (CLC) map Copernicus Program, and the Urban Atlas, 2018. The CORINE 2012 program contains land cover data for Europe including land cover classes published by the European Commission. The European Urban Atlas provides reliable, high-resolution land use maps for more than 300 large urban zones [39,40]. For the necessities of this study, the Urban Atlas, 2018 was used to map the urban and burned areas while the CORINE 2012 was utilized to identify the rest of the land uses. The land uses, which reflect the vegetation covering, were classified into six categories as follows: (i) urban area, (ii) cropland, (iii) woodland, (iv) shrubland and grassland, (v) sparse vegetation area and (vi) burned area ( Figure 4B). The urban and burned areas covered 33% and 22% respectively of the whole study area, while the remaining area consisted of 1% cropland, 5% woodland, 5% shrubland and grassland and 34% sparse vegetation.

The Rating of Every Class and the Weighting of the Factors
Each class of the involved factors had to be normalized to a standard rating scale. The determination of the rating of the classes was based on published work [32,46,47] and personal experience from previous studies of flood activity.
A five-grade scale was used for the normalization of the classes. Positive, whole numbers, ranging from 0 to 4, were given to every class. Each class expresses a different hazard level. Thus, the class rated as 0 expresses a low flood hazard, while the class rated as 4 expresses a high flood hazard. Table 1 shows the factors, their classes and their ratings.

Land Cover
Since the vegetation can help absorb rainfall, land cover influences the occurrence of floods. Since high-resolution land use data of the study area were not available, the land cover of the study area was taken from the CORINE 2012 Land Cover (CLC) map Copernicus Program, and the Urban Atlas, 2018. The CORINE 2012 program contains land cover data for Europe including land cover classes published by the European Commission. The European Urban Atlas provides reliable, high-resolution land use maps for more than 300 large urban zones [39,40]. For the necessities of this study, the Urban Atlas, 2018 was used to map the urban and burned areas while the CORINE 2012 was utilized to identify the rest of the land uses. The land uses, which reflect the vegetation covering, were classified into six categories as follows: (i) urban area, (ii) cropland, (iii) woodland, (iv) shrubland and grassland, (v) sparse vegetation area and (vi) burned area ( Figure 4B). The urban and burned areas covered 33% and 22% respectively of the whole study area, while the remaining area consisted of 1% cropland, 5% woodland, 5% shrubland and grassland and 34% sparse vegetation.

The Rating of Every Class and the Weighting of the Factors
Each class of the involved factors had to be normalized to a standard rating scale. The determination of the rating of the classes was based on published work [32,46,47] and personal experience from previous studies of flood activity.
A five-grade scale was used for the normalization of the classes. Positive, whole numbers, ranging from 0 to 4, were given to every class. Each class expresses a different hazard level. Thus, the class rated as 0 expresses a low flood hazard, while the class rated as 4 expresses a high flood hazard. Table 1 shows the factors, their classes and their ratings.  Table 2 shows the weights of every involved factor in flood hazard assessment. The CR was calculated to check the table-matrix and the valuation of the factors. It was found to be 0.04, so the decisions which are represented in Table 2 were well estimated.

The Flood Hazard Index Values and the Uncertainty
The flood hazard index values (FI) were commutated by using Equation (1): where n is the number of factors, R i is the rating of factor i and W i is the weight of factor i. Thus, the basic flood hazard assessment map was produced. Uncertainty has an important role in natural hazard evaluation [49,53]. Uncertainties in the weights of the adopted factors can bias the outcome of every hazard assessment. Published works [32,36,37,46,47], where geoenvironmental factors were evaluated through the AHP method, were used to calculate the uncertainties, ∆W i , of the weighting coefficient. The values of the weighting coefficient which are presented in Table 2 were changed by 20%. The new weight values (∆W i ) of every factor are shown in Table 3.
The values of the error map were multiplied by 1.96 to calculate the 95% confidence level of the flood hazard values and in the next step, were added and subtracted from the basic flood hazard values. Thus, two other maps characterizing the maximum and minimum flood hazard values were produced.

Verification and Correlation of the Flood Hazard Evaluation
The accuracy of the actual hazard level was examined by using past flood events. They were included in published works [32], and the historical flood database of Greece [41]. A flood inventory map was generated which includes nine flood occurrences that were observed in the municipality unit of Nea Makri for the period 2000-2020 ( Figure 5). The verification was based on the statistical analysis of the frequency ratio (FR) method. It expresses the association between the spatial distribution of floods and hazard zones. In the published works [11,32,54,55], the methodology of the calculation of the FR area is presented.
Finally, the zones of the basic flood hazard map were compared with the active urban fabric and road network of the study area.

Results
The implementation of the previously described flood hazard assessment method led to the production of three flood hazard maps. The standard deviation method was used to categorize the maps. The areas of the maps were categorized into five classes, which were very high, high, moderate, low and very low flood hazard. Figure 6 illustrates the basic flood hazard assessment map (FHb). In this map, the areas of very high and high flood hazard are located primarily in lowlands and particularly in eastern and southern parts of the study area. The moderate hazard zone is distributed mainly in the central part and the eastern and southern parts of the map. In the northern and western parts of the study area, many locations are situated in low and very low hazard areas. The verification was based on the statistical analysis of the frequency ratio (FR) method. It expresses the association between the spatial distribution of floods and hazard zones. In the published works [11,32,54,55], the methodology of the calculation of the FR area is presented.
Finally, the zones of the basic flood hazard map were compared with the active urban fabric and road network of the study area.

Results
The implementation of the previously described flood hazard assessment method led to the production of three flood hazard maps. The standard deviation method was used to categorize the maps. The areas of the maps were categorized into five classes, which were very high, high, moderate, low and very low flood hazard. Figure 6 illustrates the basic flood hazard assessment map (FHb). In this map, the areas of very high and high flood hazard are located primarily in lowlands and particularly in eastern and southern parts of the study area. The moderate hazard zone is distributed mainly in the central part and the eastern and southern parts of the map. In the northern and western parts of the study area, many locations are situated in low and very low hazard areas.      Figure 7A,B demonstrates the maximum and minimum value of each pixel's flood hazard assessment, respectively, after considering the uncertainty in the weighting coefficients. According to the flood hazard analysis, the northeastern eastern and southeastern parts of the study area host the most flood-prone regions.  The percentages corresponding to the area of each hazard zone for the three maps of Figures 6 and 7 are tabulated in Table 4. In the areas of the high and very high zones of the map with the upper flood hazard (FHmax), values slightly increased compared to the corresponding zones of the basic map (FH). The similar correlation proves that the spatial extents of moderate and low hazard zones decreased, while the very low hazard zone increase. Comparing the zones of the map with the lower flood hazard values (FHmin) to those of the basic map (FH), the areas of very high and high hazard zones showed a little increase, the moderate and low hazard areas slightly decreased, while the area of very low hazard zone remained unchanged. Table 4. Percentages represent the area of each flood hazard zone (areas are shown in Figures 6  and 7).  Table 5 tabulates the estimated frequency ratio of the flood events for each flood hazard zone. According to [54][55][56], when the ratio values are more than 1, then there is a strong relationship between events and the given natural hazard zone.   Table 5 shows that flood events were significantly correlated to very high and high hazard zones. In the very high hazard area, the frequency ratio was higher than 2, demonstrating a very high probability of flooding. Similarly, the ratio value was observed to be 1.7, in the high hazard zone, showing a high likelihood of flood occurrences. Because the ratio value was lower than 1 in the moderate hazard zone, the probability of floods is low. Since the ratio value was found to be equal to 0 in the low and the very low hazard zones, the likelihood of flooding is minimal.

Flood Hazard Zones
Moreover, the urban area and the road network were superimposed on the basic flood hazard map. In this context, the area of the urban fabric and the length of the road network that overlaps into each flood hazard zone were estimated (Table 6). The results demonstrate that the vast majority of the urban areas are located within very high and high flood hazard zones. Half of the road network's total length is situated within very high and high flood hazard zones. In contrast, small parts of the urban fabric and the other half of the road network are located within very low, moderate and low landslide hazard zones.

Discussion
The urban area constitutes about 33% of the entire study area. The study area has suffered from urban fires in 2018, resulting in about 25% of the area being burned. According to Fox [21], Euro-Mediterranean countries have common post-fire risk characteristics. They have relatively high population densities, and much of the coastal lowland area is developed. Hence, even small fires can be hazardous, and after fire these coastal areas are vulnerable to flooding. So since the study area is a coastal area and more than half of it is occupied by urban and burned areas, is at high risk of flooding.
In the present study, a method is presented to assess the flood hazard in burned areas and it can be applied even outside the localities affected by the fire. It provides an estimation of flood-prone areas where data are not available, which are typically used more often in connection with floods. Six physical and anthropogenic factors were considered as the most relevant parameters affecting the watercourse when intense storm events cause high runoff that exceeds drainage system capacity. The physical factors, related to flood activity, were slope, elevation, distance from open channel streams, and hydrolithology. The anthropogenic factors associated with floods were distance from totally covered streams, along with burnt and urban areas derived from land cover, as well as supplementary land uses.
A flood hazard assessment map was created via the AHP method and a GIS. According to Hervás and Bobrowsky [57], flood hazard refers to the probability of flood occurrence within a reference period of time. In the present study, the link of the flood hazard assessment to return periods was not possible. So, a flood susceptibility map was produced which refers to the spatial likelihood or probability for a flood to occur in the future. This map represents the potential flood hazard in the study area, and was further categorized by using the standard deviation method with five classes (Figure 6) of hazard level: very low, low, moderate, high and very high.
The areas of flood hazard varying between very high and high were recorded mostly in the eastern and southern parts of the Nea Makri area. The area of these two hazard zones covers almost 40% of the whole area (Table 4). In Greece, extreme flash flood events of low frequency and high magnitude occur in many fluvial systems with a relatively small extent drained by ephemeral streams [58]. Thus, the small drainage basins, along with the torrential behavior of the streams, influence the flood manifestations in the study area. Moreover, the lowland morphology, gentle slope, the covered streams and intense urbanization in the eastern part of the municipality unit of Nea Makri increase the runoff and produce encouraging locations for flood occurrences. According to Shakesby [59], in Euro-Mediterranean regions wildfires in forests leave the terrain bare and vulnerable to storms which can cause severe runoff and soil erosion. The runoff increases often in the upper parts of watersheds, and thus poses flooding risks in urban zones located downstream. Thus, the burned area in the southern part of the study area creates favorable conditions for flooding.
In contrast, low and very low flood hazard areas are situated in the mountainous northern, northwestern and western parts of the municipality unit of Nea Makri. These areas are not urbanized, contain open stream channels and do not include burned areas. Therefore, the hazard of flooding in these areas is very low. The spatial distribution of the moderate hazard zone is observed primarily in the central, eastern and southern parts of the municipality unit of Nea Makri. These three hazard zones cover almost 60% of the whole area (Table 4).
The AHP method is a powerful and valuable tool for flood hazard analysis [32,36,46,47], although it shows several constraints in assessing the impact of uncertainties [60,61]. This fact was evaluated by calculating two additional scenarios that present the upper and lower flood hazard values after accounting for the uncertainty in the weighting coefficients (Table 3). The findings of the uncertainty analysis showed that the two additional maps (FHmin and FHmax) illustrate a low variation of the presence of flood hazard zones (Table 5) concerning the basic flood hazard map (FHb). Consequently, the analysis proved slight differences in the spatial and quantitative distribution of the flood hazard zones. This fact indicates robust behavior for the predictions of the applied method.
The combination of several different maps can create a map that does not contain an area's actual hazard level [62]. Thus, the basic flood hazard map was verified by means of frequency ratio and flood events which affected the study area over the past 20 years. The findings established that the vast majority of the floods, almost 90% (Table 5), were located within the limits of the high and very high flood hazard zones. Moreover, the frequency ratio was higher than 1 in the high and very high hazard zones, indicating that these hazard zones are strongly correlated with flood occurrences ( Table 5). The flood hazard intensity rises as the frequency ratio values increase.
The applied method brings many advantages; first of all, that of offering completeness of the analysis of the territory and methodological homogeneity. It is simple and easy to use where primary data are scarce. The results provide reasonable values, which could lead to its further application. The used approach is, therefore, useful in synergy with methods linked to the attribution of a probability.
Comparing the existing urban fabric and road network to the proposed hazard areas of the basic flood hazard map, it is recorded that the vast majority (77%) of the urban fabric and 50% of the road network's length are situated within the boundaries of high and very high flood hazard zones (Table 6). This result demonstrated that they have been constructed in areas prone to flood. In these areas, proactive planning and selection of the proper construction rules are essential for the prevention and mitigation of the consequences of flood hazards.
Detailed works relating to the condition of events and evolution of natural hazards and the vulnerability of the exposed elements at risk (i.e., buildings) will help propose the proper protection measures [46]. The application of the procedure facilitates identifying those sites from the already existing urban fabric and road network situated in non-safe areas. Thus, the appropriate mitigation or hazard reduction approaches can be more effectively designed and applied. Furthermore, the awareness of the non-safe regions related to flood hazard might be helpful in emergency preparedness planning. Therefore, scientists, engineers, stakeholders, planners and decision makers may utilize the proposed approach in forthcoming spatial planning projects [63][64][65][66][67][68]. Additionally, the local authorities may use the produced map to guide the adoption of measures and strategies aiming towards flood hazard mitigation and post-fire management.

Conclusions
In the present work, a burned and urban area of the Attica peninsula in central Greece was selected to produce a flood hazard assessment map. The proposed areas of very high and high flood hazard are located mainly in the study area's eastern and southern parts as a consequence of the synthesis of lowlands with gentle slope, ephemeral streams with torrential behavior, totally covered streams and urban areas. The burned area in southern part of the study area will increase surface runoff and create favorable conditions for flooding. The uncertainty analysis showed insignificant variations of the spatial distribution of the flood hazard zones. The flood hazard map presents a significant correlation between the flood hazard zones and the spatial distribution of flood phenomena. This verification demonstrated reliable results and high accuracy of the created map. The spatial distribution of the existent urban fabric and road network was analyzed to identify the parts situated in unsafe areas to design and apply flood hazard mitigation measures. About 80% of the urban areas and 50% of the road network's length were located within areas prone to flood. The proposed method offers completeness of the analysis of the territory, is simple to apply where primary data are scarce and provides reasonable results, which could lead to its further application. Therefore, scientists, stakeholders, engineers and decision makers may apply the proposed approach in forthcoming land use planning projects. Flood hazard mitigation techniques can be more effectively designed, while the proposed approach may be useful also in emergency preparedness planning and post-fire management.

Data Availability Statement:
Data that support the findings of this study are available from the corresponding author upon reasonable request.