Abstract
Flash floods are phenomena in which the important hydrologic processes are occurring on the same spatial and temporal scales as the intense precipitation. To date, the time required for appropriate public response has typically been much longer than the time between the causative precipitation and the subsequent flash flood. The impact of a flash flood is primarily related to the sudden increase in level and velocity of floodwater, rather than the peak level and velocity, or the final duration and extent of the floodwater. The impact of rapidly evolving precipitation systems on the complex hydrologic processes of fast-response basins makes the flash flood phenomenon a particularly challenging forecast problem.
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Kelsch, M., Caporali, E., Lanza, L.G. (2001). Hydrometeorology of Flash Floods. In: Gruntfest, E., Handmer, J. (eds) Coping With Flash Floods. NATO Science Series, vol 77. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-0918-8_4
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DOI: https://doi.org/10.1007/978-94-010-0918-8_4
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