Análisis y comportamiento espacial de la fractalidad temporal de la precipitación en la españa peninsular y baleares (1997-2010)

The temporal fractality of rainfall 'D' indicates the property of self-Similarity of rain, rainy events that recur regularly at different time scales. D values are determined for 44 stations of mainland Spain and the Balearic Islands, varying between 1.6039 and 1.4499. According semesters, D values are lower in the warm half of the year than in the cold half. In the north, D values are higher, annual and semi-Annual, whereas in the Eastern coast and Baleares and in the Ebro valley are lower, and higher differences between D values of both warm and cold halves in the north and the Guadalquivir valley.