Uncertanly assesment in the prediction of extreme rainfall events: an example from the Central Spanish Pyrenees

  1. García-Ruiz, J.M. 2
  2. Arnáez, J. 1
  3. White, S.M. 3
  4. Lorente, A. 2
  5. Beguería, S. 2
  1. 1 Universidad de La Rioja
    info

    Universidad de La Rioja

    Logroño, España

    ROR https://ror.org/0553yr311

  2. 2 Instituto Pirenaico de Ecología
    info

    Instituto Pirenaico de Ecología

    Zaragoza, España

    ROR https://ror.org/039ssy097

  3. 3 Durham University
    info

    Durham University

    Durham, Reino Unido

    ROR https://ror.org/01v29qb04

Revista:
Hydrological processes

ISSN: 0885-6087

Año de publicación: 2000

Volumen: 14

Número: 5

Páginas: 887-898

Tipo: Artículo

DOI: 10.1002/(SICI)1099-1085(20000415)14:5<887::AID-HYP976>3.0.CO;2-0 SCOPUS: 2-s2.0-0342369598 WoS: WOS:000086843900004 GOOGLE SCHOLAR

Otras publicaciones en: Hydrological processes

Repositorio institucional: lock_openAcceso abierto Editor

Resumen

Extreme rainfall events occur frequently in the central Pyrenees, but they are responsible for mass movements and short, very intense erosion periods, accompanied at times by loss of human and high costs of infrastructure. This paper tries to assess the existence of patterns in the spatial distribution of maximum precipitation. The calculation of return periods of the most intense rainfall demonstrates that in the Pyrenees it exhibits an erratic spatial and temporal distribution and can be extremely localized. In the case of precipitation between 150 and 200 mm in 24 h, some influence from the surrounding relief has been found, but this is not the case for precipitation exceeding 200 mm, characterized by the absence of patterns governing their spatial distribution. Geomorphological approaches are, therefore, the only way for assessing the areas more subject to hydromorphological risks. Copyright (C) 2000 John Wiley and Sons, Ltd.Extreme rainfall events occur frequently in the central Pyrenees, but they are responsible for mass movements and short, very intense erosion periods, accompanied at times by loss of human life and high costs of infrastructure. This paper tries to assess the existence of patterns in the spatial distribution of maximum precipitation. The calculation of return periods of the most intense rainfall demonstrates that in the Pyrenees it exhibits an erratic spatial and temporal distribution and can be extremely localized. In the case of precipitation between 150 and 200 mm in 24 h, some influence from the surrounding relief has been found, but this is not the case for precipitation exceeding 200 mm, characterized by the absence of patterns governing their spatial distribution. Geomorphological approaches are, therefore, the only way for assessing the areas more subject to hydromorphological risks.