Articles | Volume 15, issue 8
https://doi.org/10.5194/nhess-15-1859-2015
https://doi.org/10.5194/nhess-15-1859-2015
Research article
 | 
19 Aug 2015
Research article |  | 19 Aug 2015

Flash flood occurrence and relation to the rainfall hazard in a highly urbanized area

K. Papagiannaki, K. Lagouvardos, V. Kotroni, and A. Bezes

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Cited articles

Amaro, J., Gayà, M., Aran, M., and Llasat, M. C.: Preliminary results of the Social Impact Research Group of MEDEX: the request database (2000–2002) of two Meteorological Services, Nat. Hazards Earth Syst. Sci., 10, 2643–2652, https://doi.org/10.5194/nhess-10-2643-2010, 2010.
Barberia, L., Amaro, J., Aran, M., and Llasat, M. C.: Social impact analysis of two heavy rain events in Catalonia: 14 and 15 July 2001 and 3 April 2002, Plinius Conference on Mediterranean Storms, Disasters and Climate Change: knowing how to adapt, Savona, Italy, 7–9 September 2011, Programme Book, contribution 13–57, 2011.
Barbería, L., Amaro, J., Aran, M., and Llasat, M. C.: The role of different factors related to social impact of heavy rain events: considerations about the intensity thresholds in densely populated areas, Nat. Hazards Earth Syst. Sci., 14, 1843–1852, https://doi.org/10.5194/nhess-14-1843-2014, 2014.
Barrera-Escoda, A. and Llasat, M. C.: Evolving flood patterns in a Mediterranean region (1301–2012) and climatic factors – the case of Catalonia, Hydrol. Earth Syst. Sci., 19, 465–483, https://doi.org/10.5194/hess-19-465-2015, 2015.
Bracken, L. J., Cox, N. J., and Shannon, J.: The relationship between rainfall inputs and flood generation in south–east Spain, Hydrol. Process., 22, 683–696, https://doi.org/10.1002/hyp.6641, 2008.
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Short summary
48 flash flood events in the urban Attica region (2005-2014) resulted in 3,500 fire service operations, mostly in autumn. Events were mostly associated with max accumulated rain over 20mm/24h and 3mm/10min. Impact intensity was particularly high for more than 60mm/24h. Rain intensity thresholds for flood triggering are produced for 15 sub-areas of the Attica region. The quality of the produced thresholds depends on the distribution and density of the rain gauges that cover each sub-area.
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