Characterization of high-intensity storms in the Metropolitan Area of Barcelona (2014–2022)

Data de publicació

2026-03-24T15:42:13Z

2026-03-24T15:42:13Z

2025-12-28

2026-03-24T15:42:15Z



Resum

Urban coastal areas along the Mediterranean are exposed to short-duration convective rainfall, producing infrastructure disruptions and flood-related impacts. This study analyzes 45 rainfall episodes in the Metropolitan Area of Barcelona between 2014 and 2022, combining radar products, rain gauge observations, and urban-scale impact datasets. Storm radar tracking enabled the identification of key spatiotemporal features and assessment of short-term forecasting performance. Convective cells were typically short-lived, lasting less than 30 min in most cases. The main goal of the research has been the comparison between VIL density (DVIL) radar field and short-duration rainfall intensity provided by rain gauges. This is the first study comparing both data types, being a pioneer in this field. We have found a linear relationship between both data types, with weaker values for larger values. More persistent cells had higher DVIL values, observing a difference in behavior with a break point at 2 g/m3. The tracking and nowcasting system were evaluated based on its ability to anticipate convective precipitation. It achieved good scores values (POD of 0.73 and FAR of 0.33), considering the difficulties of tracking this type of convective system. Finally, false alarms associated with elevated DVIL values suggested the difficulty of capturing storm severity by surface-based precipitation measurements.measurements.

Tipus de document

Article


Versió publicada

Llengua

Anglès

Matèries i paraules clau

Tempestes; Pluja; Radar; Storms; Rain and rainfall; Radar

Publicat per

MDPI

Documents relacionats

Reproducció del document publicat a: https://doi.org/10.3390/atmos17010041

Atmosphere, 2025, vol. 17, p. 1-20

https://doi.org/10.3390/atmos17010041

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Drets

cc-by (c) Esbrí et al., 2025

http://creativecommons.org/licenses/by/4.0/

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