Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index

Author:

Aleksova Bojana1,Milevski Ivica2,Mijalov Risto2,Marković Slobodan B.34,Cvetković Vladimir M.567,Lukić Tin3

Affiliation:

1. Maarif International School – Skopje Campus , Kiro Gligorov 5, 1000 , Skopje , North Macedonia

2. Institute of Geography, Faculty of Natural Sciences and Mathematics, Ss. Cyril and Methodius University , Arhimedova 3, 1000 , Skopje , North Macedonia

3. Department of Geography, Tourism and Hotel Management, Faculty of Sciences, University of Novi Sad , Trg Dositeja Obradovića 3, 21000 , Novi Sad , Serbia

4. Serbian Academy of Sciences and Arts , Kneza Mihaila 35, 11000 , Belgrade , Serbia

5. Faculty of Security Studies, University of Belgrade , Gospodara Vucica 50, 11040 , Belgrade , Serbia

6. Scientific - Professional Society for Disaster Risk Management , Dimitrija Tucovića 121, 11040 , Belgrade , Serbia

7. International Institute for Disaster Research , Dimitrija Tucovića 121, 11040 , Belgrade , Serbia

Abstract

Abstract This study presents a comprehensive analysis of flash flood susceptibility in the Kratovska Reka catchment area of Northeastern North Macedonia, integrating Geographic Information System, remote sensing, and field survey data. Key factors influencing flash flood dynamics, including Slope, Lithology, Land use, and Vegetation index, were investigated to develop the Flash Flood Potential Index (FFPI). Mapping slope variation using a 5-m Digital Elevation Model (DEM) revealed higher slopes in eastern tributaries compared to western counterparts. Lithological units were classified based on susceptibility to erosion processes, with clastic sediments identified as most prone to flash floods. Land use analysis highlighted non-irrigated agricultural surfaces and areas with sparse vegetation as highly susceptible. Integration of these factors into the FFPI model provided insights into flash flood susceptibility, with results indicating a medium risk across the catchment. The average value of the FFPI is 1.9, considering that the values range from 1 to 5. Also, terrains susceptible to flash floods were found to be 49.34%, classified as medium risk. Field survey data validated the model, revealing a significant overlap between hotspot areas for flash floods and high-risk regions identified by the FFPI. An average FFPI coefficient was calculated for each tributary (sub-catchment) of the Kratovska Reka. According to the model, Latišnica had the highest average coefficient of susceptibility to potential flash floods, with a value of 2.16. These findings offer valuable insights for spatial planning and flood risk management, with implications for both local and national-scale applications. Future research directions include incorporating machine learning techniques to enhance modeling accuracy and reduce subjectivity in assigning weighting factors.

Publisher

Walter de Gruyter GmbH

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