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This study shows that the relationships between rainfall and runoff at the event scale in a small farmland abandoned catchment are not linear and that the hydrological response is linked to the antecedent wetness conditions. Rainfall and baseflow discharge have a pronounce influence on the value of the runoff coef23 Cuadernos de Investigacion Geografica 2008 No 34 pp. 23-37 ISSN 0211-6820 © Universidad de La Rioja ficient, while rainfall intensity affects the maximum discharge increment. Watertable data show high seasonal dynamics, with a dry period during summer, a wet period during winter and spring, and a transition period characterised by a high spatial variability. The analysis of the hydrological information at the event scale allows the distinction of three types of event, and reveals the occurrence of different runoff generation processes within the catchment. During dry conditions, the hydrological response is very low and infiltration excess over localised areas is likely to be the main runoff process. As the catchment gets wetter, saturated excess runoff (and probably subsurface flow) becomes the dominant runoff process. Palabras clave: relaciones precipitacion-escorrentia; nivel freatico; estacionalidad; cuenca experimental; Pirineo Central

Diferencias estacionales en la generación de escorrentía en una pequeña cuenca de campos abandonados en el Pirineo Central