Articles | Volume 12, issue 4
Nat. Hazards Earth Syst. Sci., 12, 881–891, 2012
https://doi.org/10.5194/nhess-12-881-2012

Special issue: 12th Plinius Conference on Mediterranean Storms

Nat. Hazards Earth Syst. Sci., 12, 881–891, 2012
https://doi.org/10.5194/nhess-12-881-2012

Research article 10 Apr 2012

Research article | 10 Apr 2012

Lightning activity, rainfall and flash flooding – occasional or interrelated events? A case study in the island of Crete

A. G. Koutroulis1, M. G. Grillakis1, I. K. Tsanis1,2, V. Kotroni3, and K. Lagouvardos3 A. G. Koutroulis et al.
  • 1Water Resources Management and Coastal Engineering Laboratory, Environmental Engineering Dept., Technical University of Crete, Greece
  • 2Department of Civil Engineering, McMaster University, Hamilton, Canada (on research leave)
  • 3Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Greece

Abstract. The majority of cyclones passing over Crete in late autumn to early winter originate from southwest, west and northwest and are of varying size and intensity. A number of these cyclones cause flash floods. The present study reports the possible relationships between lighting activity and high precipitation related to flash flood events. In this study an attempt was made to correlate the lightning number and location, recorded by the ZEUS lightning detection system, with the rainfall characteristics for sixteen rain events (4 flood and 12 non-flood events) on the island of Crete, during the period 2008–2009. Spatiotemporal analysis of rain and rain rate with flash count was performed with respect to distance (radius) of flashes from raingauge location at various temporal scales, in order to examine the correlation of accumulated rainfall and lightning activity. The maximum attained statistical significant correlation was obtained within a circular area of an average radius of 15 km around the raingauge, and an average time lag of flash count prior precipitation accumulation of 15 min. The maximum correlation between the lightning and rainfall data is obtained for shorter time lags for the flood events (15 min) than the non-flood events (25 min), that could reflect the faster propagation of flood triggering storms due to high convective activity. Results show increased lightning activity occurring during flood triggering storms, by an average of four times higher. Furthermore, there is evidence that the number of flashes that occur during a precipitation event is related to precipitation depth when the latter is adequate to produce a flood event. Differences between flood and non-flood producing storms need to be further assessed by analyzing more independent parameters, including the synoptic conditions and dominant flash flood hydrological generating processes.

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