EGU26-20102, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-20102
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Monday, 04 May, 17:40–17:50 (CEST)
 
Room 2.31
Flood Warnings Risks: Spatial and Temporal Distribution of Flood Warning Alerts in London
Nicola Cekalska and Kourosh Behzadian
Nicola Cekalska and Kourosh Behzadian
  • School of Computing and Engineering, University of West London, St Mary's Rd, London, W5 5RF, UK (nicolalska@hotmail.com)

The growing reliance on early flood warning systems reflects broader advances in real-time flood forecasting, where increasing data availability, modelling complexity, and the integration of data-driven and AI-based approaches have been identified as critical enablers for effective urban flood risk management [1]. To investigate if flood warning distribution is affected by hydrological variables, socioeconomic vulnerabilities or physical exposure, this study evaluates the spatial and temporal trends of the Environment Agency (EA)’s flood warnings between 2006-2024 within London boroughs.

By applying a comprehensive methodology incorporating GIS analysis, socioeconomic correlation analysis and time-series integration, Flood Alert (FA), Flood Warning (FW) and Severe Flood Warning (SFW) data were analysed using EA’s open-access data. Significant spatial variations were identified within the analysis. Riparian boroughs along the River Thames corridor experienced significantly higher FW rates (>293 alerts per borough approximately per year) compared to non-riparian boroughs (<80 alerts per borough), implying that hydraulic exposure was the primary source of flooding. Temporal analysis presented significant winter seasonality, with approximately 55% of total FW distributed between 2006-2024 confirming limited soil moisture conditions and Atlantic-driven storm activity. Summer FA’s decreased within recent years despite climate change predictions estimating increased convective rainfall, indicating either potential inadequate warning levels of pluvial risks or enhanced operational discrimination.

Regardless of population and exposure controls, distribution analysis presented severe equality implications. London boroughs with increased deprivation projected disproportionately higher FW effects per capita. The trend remained consistent throughout the study period, demonstrating compound vulnerability across the intersection of reduced adaptive capacity and physical hazard exposure. Identifying specific city hotspots (Newham, Tower Hamlets, Southwark) involving higher FA, FW, SFW frequencies occurring simultaneously with socio-economic disadvantages, aging drainage systems and limited green infrastructure.

Findings suggest the requirement for change in policy and procedures for flood risk management, including the development of locally adapted, topography-specific operational guidelines for hydrologically maintained confluence zones; improved accountability via open reporting of operational metrics for lead times and false alarm rates; increased socioeconomically inclusive flood communication strategies, prioritising the engagement of vulnerable communities; improved monitoring design to mitigate coverage gaps; and adoption of comprehensive flood risk frameworks, integrating socioeconomic vulnerability risk assessments with physical exposure controls.

This study enrichens the understanding of operations of urban flood warning systems with complex socioeconomic and technical environments. The methodology and research findings demonstrate reproducible procedures for the analysis of operational flood warning systems within local and regional scales, promoting evidence-based advancements in urban resilience planning in accordance with UK Flood and Water Management Act 2010 and EU Floods Directive (2007/60/EC).

How to cite: Cekalska, N. and Behzadian, K.: Flood Warnings Risks: Spatial and Temporal Distribution of Flood Warning Alerts in London, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-20102, https://doi.org/10.5194/egusphere-egu26-20102, 2026.