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

  1. Óliver Meseguer-Ruiz
  2. Javier Martín-Vide
  3. Jorge Olcina Cantos
  4. Pablo Sarricolea
Revista:
BAGE. Boletín de la Asociación Española de Geografía

ISSN: 0212-9426

Año de publicación: 2017

Número: 73

Páginas: 11-32

Tipo: Artículo

DOI: 10.21138/BAGE.2407 DIALNET GOOGLE SCHOLAR

Otras publicaciones en: BAGE. Boletín de la Asociación Española de Geografía

Resumen

La fractalidad temporal de la precipitación ‘D’ indica la característica de autosimilitud de la lluvia, el hecho que los sucesos lluviosos se repitan con regularidad a diferentes escalas temporales. Los valores de D se determinan para 44 estaciones de la España peninsular y Baleares, variando entre 1,6039 y 1,4499. Según semestres, los valores de D son más bajos en la mitad cálida del año que en la mitad fría. En el norte los valores de D son mayores, a nivel anual y semestral, mientras que en la fachada oriental y Baleares y en el valle del Ebro son menores, y las mayores diferencias entre los valores de D delos periodos cálido y frío se dan en el norte y en el valle del Guadalquivir.

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Fuente de los datos: Dialnet