💧 Flood Damage
JRC depth-damage curve applied to building footprints and critical infrastructure. Flood depth drives both hazard scoring and vulnerability fraction. Return periods: 10yr, 100yr, 500yr.
The Fiscal Threat: Translating Water Depth to Financial Loss
Flooding is the temporary inundation of land not normally covered by water. Flood types include riverine flooding (overbank flow from rivers), pluvial flooding (surface runoff from intense precipitation exceeding drainage capacity), coastal flooding (storm surge combined with sea-level rise), and flash flooding (rapid-onset inundation in steep or small catchments).
The ClimEmpower flood assessment translates flood depth into financial damage through the JRC depth-damage function (Huizinga et al., 2017). This moves beyond binary flood/no-flood mapping to produce a monetised vulnerability score per grid cell — directly usable by municipal planners and insurers. A displacement threshold of 0.5 metres flood depth is applied as the evacuation trigger for population risk.
The assessment combines a mapped climate hazard with the people, assets or ecosystems exposed to it and their vulnerability. Sector-specific indicators then produce the final risk result.
Vulnerability function V = f(depth) · Monetary loss fraction 0–1
< 0.1 mNegligible< 5%0.1–0.5 mLow5–18%0.5–1.0 mModerate18–35%1.0–2.0 mHigh35–52%2.0–3.0 mVery High52–71%> 3.0 mExtreme> 71%JRC depth-damage curve applied to building footprints and critical infrastructure. Flood depth drives both hazard scoring and vulnerability fraction. Return periods: 10yr, 100yr, 500yr.
Composite result of Hazard × Exposure × Vulnerability, expressed on a common 1–1,000 scale.
Limited risk. Maintain existing good practices.
Low impact. Maintain adaptive capacity.
Noticeable risk. Precautionary planning is recommended.
Significant risk. Targeted intervention is needed.
Severe risk. Immediate action is required.
R_flood = H × E × VFlood depth — 10-year return period
JRC EFAS · Copernicus EMS · 100mFlood depth — 100-year return period
JRC EFAS · Copernicus EMS · 100mFlood depth — 500-year return period
JRC EFAS · Copernicus EMS · 100mBuilding footprints (residential, commercial, industrial)
OpenStreetMap / Local cadaster · Building-levelCritical infrastructure (transport, energy, water treatment) in flood zone
Eurostat GISCO · OpenStreetMap · GeofabrikJRC depth-damage function: monetary loss fraction 0–1, scored 1–10 (<0.1m=1, 0.1–0.5m≈3, 0.5–1m≈5, 1–2m≈7, >2m=10)
Huizinga et al. (2017) · JRC flood damage model · Building-levelBuilding material and age (masonry > concrete in vulnerability)
Local cadaster / EMS damage models · Building-levelReturn periods 10yr, 100yr, 500yr. Depth maps.
99th percentile events. RCP4.5 and RCP8.5.
Secondary indicator for flood accumulation zones.
Primary exposure for Flood Damage index.
Transport, energy, water treatment in flood zones.
<0.1m=1 → >2m=10. Monetary loss fraction 0–1.
Masonry > concrete in flood vulnerability.
Steeper terrain = higher flow velocity = more stress.
Andalusia faces compound flood risk from multiple sources: riverine flooding along the Guadalquivir and Genil, flash flooding in the Ramblas of Almería and Málaga, and coastal flooding along the delta and estuarine zones. High-resolution flood hazard maps from the Guadalquivir River Authority and building-level cadaster data are available for this region, going well beyond the pan-European JRC datasets. A more elaborate risk calculation method has been established to make full use of this data.
The Andalusian method also places greater emphasis on Vulnerability over Hazard and Exposure, since this is the factor the region can influence most efficiently. This is reflected in the following risk calculation formula.
CHG Guadalquivir maps used for RP10/RP100 in the main basin (higher resolution than JRC). DANA-type events have shifted RP100 estimates upward in Málaga/Jaén ramblas — model updated with post-event survey.
No flood / < 0.1m1No hazard0.1–0.5m3Low (wading depth)0.5–1.0m5Moderate (displacement trigger)1.0–2.0m7High> 2.0m10Extreme (structural damage)Andalusia's Ramblas (ephemeral rivers in Almería/Málaga) experience flash-flood events of 200+ mm/24h. AEMET pluviometric stations are dense enough to downscale EPI to 5km for these catchments.
< 50 mm/24h at P992Low EPI50–1004Moderate100–1506High (Ramblas trigger)150–2008Very high> 200 mm/24h10Extreme (DANA-type)Spanish Catastro provides construction year, floor count, and declared use for every building. This replaces generic OSM footprints and allows building-age vulnerability differentiation (pre-1980 masonry most vulnerable).
No buildings in flood zone1No exposure< 10 buildings/100m cell3Sparse10–50 buildings/100m5Residential50–2007Dense residential> 200 buildings or critical infra.10Critical exposureCHG post-2024 DANA survey data calibrated the generic JRC curve for Andalusian building typologies. Pre-1980 load-bearing masonry common in Guadalquivir valley shows 40% higher damage fraction than JRC generic at 1m depth.
< 5% monetary loss fraction1Negligible5–20%3Low20–40%5Moderate40–65%7High> 65% monetary loss10Extreme damageCatastro year of construction used to assign structural vulnerability class: pre-1940 adobe/rubble = 10; 1940–1980 unreinforced masonry = 8; 1980–2000 confined masonry = 5; post-2000 RC frame = 3.
Post-2000 RC frame2Modern / resilient1980–2000 confined masonry4Standard1940–1980 masonry7VulnerablePre-1940 traditional9Very vulnerablePre-1940 adobe / rubble10Extreme vulnerabilityOfficial flood hazard maps for RP10/RP100/RP500 at 5–25m resolution for Guadalquivir basin
Building-level register: footprint, floor area, year built, construction type, declared use for all of Spain
Dense station network in Andalusia for DANA-event EPI calibration and 99th-percentile exceedance mapping
Andalusia's Flood Risk Management Plan (Planes de Gestión del Riesgo de Inundación) — aligns with EU Floods Directive 6-year cycle
➜ Flood damage in protected areas minimised; excess water retained or diverted
Regions: OBZ, Andalusia➜ Reduces depth-damage fraction for buildings above 0.5m threshold
Regions: OBZ, Sicily➜ Reduces surface water accumulation during pluvial events
Regions: Central Greece➜ Post-flood recovery time and repair costs reduced
Regions: OBZ➜ Transport disruptions from extreme weather reduced by up to 20%
Regions: OBZ➜ Flood duration and crop losses in flood-prone areas reduced by up to 20%
Regions: OBZ➜ Urban flood risk reduced by up to 20%; water quality improved
Regions: OBZ, Sicily, Andalusia➜ Surface runoff reduced by up to 10%; reduces pluvial flood peak
Regions: OBZ, Sicily, Andalusia➜ Stormwater infiltration increased by ≥5%; pollutant loads to water bodies reduced
Regions: OBZ➜ Attenuates peak flows; provides secondary water storage for droughts
Regions: Troodos, OBZ, Andalusia➜ Reduces peak flood flows; mitigates erosion and sediment transport
Regions: Central Greece, Sicily, Andalusia➜ Reduces intensity of coastal flood surge at shoreline
Regions: Andalusia➜ Provides up-to-date hazard maps aligned with EU Floods Directive 6-year cycle
Regions: Central Greece, Andalusia➜ Enables timely evacuation above 0.5m displacement threshold
Regions: Central Greece, Andalusia➜ Reduces casualties; shortens recovery time by at least 20%
Regions: Central Greece, Sicily, Andalusia➜ Prevents new development in high-hazard flood zones; lowers future E scores
Regions: OBZ, Central Greece, Sicily➜ Improves individual flood preparedness and self-evacuation decision-making
Regions: SicilyEach measure targets one or more risk components. Governance and planning measures typically reduce Exposure (E) by keeping assets out of hazard zones. Nature-based and infrastructure measures primarily reduce Vulnerability (V). Early warning and awareness measures improve adaptive capacity — the fastest path to a lower risk score.