Hazard
The environmental trigger: severity, intensity and probability.
Navigating Hazard, Exposure, and Vulnerability for Localized Resilience.
Nine targeted risk maps with full formulas and adaptation strategies.
Risk is not just weather. It is the geographic intersection of a climatic threat, the presence of societal assets, and their inherent fragility. If exposure is zero, risk is zero.
It is the geographic intersection of a climatic threat, the presence of societal assets, and their inherent fragility.
If exposure is zero, risk is zero.The environmental trigger: severity, intensity and probability.
The physical presence of assets and people in the hazard zone.
The inherent sensitivity and lack of coping capacity of exposed assets.
Normalised Risk Index from 1 to 1000.
Balanced scientific baseline aligned with IPCC recommendations.
Prioritises vulnerability because it is the component public authorities can directly influence.
Nine risk maps are produced. The grid shows the active hazard and sector combinations.
Drought is a prolonged period of below-normal precipitation that leads to water scarcity across ecosystems, agriculture, and society. Unlike other natural hazards, it has no clear onset and accumulates slowly over months to years.
The ClimEmpower methodology distinguishes between meteorological drought and agricultural drought, with dedicated risk profiles for population and agriculture.
A heatwave is a prolonged period of abnormally high temperatures that significantly exceeds the historical norms for a given region.
The ClimEmpower model uses Land Surface Temperature to identify spatial thermal hotspots and combines this with population and vulnerability indicators.
A wildfire is an uncontrolled fire occurring in vegetated areas. It is driven by fire weather, fuel availability and ignition sources.
The ClimEmpower methodology combines the Fire Weather Index with burnable vegetation and separates risk by population, agriculture, infrastructure, biodiversity and tourism.
Flooding is the temporary inundation of land not normally covered by water. The assessment translates flood depth into financial damage through depth-damage functions.
Because risk is an equation, increasing adaptive capacity lowers vulnerability and generates a new, lower risk score after intervention.
All inputs are reclassified to a common 1β10 scale.
1 β€ Variable score β€ 10Hazard, exposure and vulnerability are calculated from their constituent variables using equal weights.
C = Ξ£ Vα΅’ Γ (1/n)The three components are multiplied.
R = H Γ E Γ VAcademic and institutional sources underlying the ClimEmpower risk map methodology, hazard science and adaptation evidence base.
BΓΌgelmayer-Blaschek, M., Hochebner, A., Gazzaneo, P., et al. (2025). Measures and strategies for increased Climate Change resilience. Deliverable D2.4. ClimEmpower Horizon Europe Project, Grant No. 101112728.
IPCC (2021). Climate Change 2021: The Physical Science Basis. Cambridge University Press.
IPCC (2022). Climate Change 2022: Impacts, Adaptation and Vulnerability. Cambridge University Press.
CarrΓ£o, H., Naumann, G., and Barbosa, P. (2016). Mapping global patterns of drought risk. Global Environmental Change, 39, 108β124.
McKee, T. B., Doesken, N. J., and Kleist, J. (1993). The relationship of drought frequency and duration to time scales.
Vicente-Serrano, S. M., BeguerΓa, S., and LΓ³pez-Moreno, J. I. (2010). A multiscalar drought index sensitive to global warming.
Robine, J. M., et al. (2008). Death toll exceeded 70,000 in Europe during the summer of 2003.
Ballester, J., et al. (2023). Heat-related mortality in Europe during the summer of 2022.
Ronnkvist, S. R., et al. (2025). Metrics of Temperature Extremes in Europe NUTS Regions (1980β2024).
Oke, T. R. (1982). The energetic basis of the urban heat island.
Van Wagner, C. E. (1987). Development and structure of the Canadian Forest Fire Weather Index System.
San-Miguel-Ayanz, J., et al. (2023). Forest Fires in Europe, Middle East and North Africa 2022.
San-Miguel-Ayanz, J., Schulte, E., Schmuck, G., and Camia, A. (2013). The European Forest Fire Information System.
Moreira, F., et al. (2011). Landscape-wildfire interactions in southern Europe.
Huizinga, J., de Moel, H., and Szewczyk, W. (2017). Global flood depth-damage functions.
Munich Re (2022). Natural disasters 2021: The year in figures.
Alfieri, L., Burek, P., Feyen, L., and Forzieri, G. (2015). Global warming increases the frequency of river floods in Europe.
Vousdoukas, M. I., et al. (2018). Global probabilistic projections of extreme sea levels.
Cardona, O. D., et al. (2012). Determinants of risk: exposure and vulnerability.
Birkmann, J. (2006). Measuring vulnerability to natural hazards: towards disaster resilient societies.