1. Analysis of extreme rainfall in the Ebre Observatory (Spain)
- Author
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A. Redaño, Núria Pérez-Zanón, J. Germán Solé, Raúl Rodríguez-Solà, Juan Carlos Peña, Anna Rius, M. Carmen Casas-Castillo, Universitat Politècnica de Catalunya. Departament de Física i Enginyeria Nuclear, and Universitat de Barcelona
- Subjects
Return period ,Atmospheric Science ,010504 meteorology & atmospheric sciences ,scaling behavior ,0208 environmental biotechnology ,Mesoscale meteorology ,02 engineering and technology ,Large range ,Meteorological observations ,01 natural sciences ,Desenvolupament humà i sostenible::Prospectiva, sistèmica i modelització [Àrees temàtiques de la UPC] ,Observatory ,probable maximum precipitation ,Precipitation (Meteorology) ,0105 earth and related environmental sciences ,Climatology ,Precipitacions (Meteorologia) ,IDF curves ,rainfall classification ,Observacions meteorològiques ,020801 environmental engineering ,Pluja ,Rain and rainfall ,extreme rainfall ,Maximum precipitation ,Climatologia ,Environmental science ,Scale (map) - Abstract
The final publication is available at Springer via http://dx.doi.org/10.1007/s00704-015-1476-0 Relationship between maximum rainfall rates for time intervals between 5 minutes and 24 hours has been studied from almost a century (1905-2003) of rainfall data registered in the Ebre Observatory (Tarragona, Spain). Intensity-duration-frequency (IDF) curves and its master equation for every return period in the location have been obtained, as well as the probable maximum precipitation (PMP) for all the considered durations. In particular, the value of the 1-day PMP has resulted 415 mm, very similar to previous estimations of this variable for the same location. Extreme rainfall events recorded in this period have been analyzed and classified according to their temporal scale. Besides the three main classes of cases corresponding to the main meteorological scales, local, mesoscale and synoptic, a fourth group constituted by complex events with high intense rates for a large range of durations has been identified also, indicating the contribution of different scale meteorological processes acting together in the origin of the rainfall. A weighted intensity index taking into account the maximum rainfall rate in representative durations of every meteorological scale has been calculated for every extreme rainfall event in order to reflect their complexity.
- Published
- 2015