dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel A 1D runoff-runon model : scale and connectivity
VerfasserIn Marie-Alice Harel, Emmanuel Mouche, Jérémy Patin, Emmanuel Ledoux
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250048858
 
Zusammenfassung
Rainfall is shared differently between runoff and infiltration depending on spatial scale. At the watershed scale, it has been observed that runoff produced at the outlet generally decreases with the size of the watershed (Cerdan et al., 2004). At plot scale, infiltration is usually modelled as an Hortonian process, but this is rigorously justified only at the core scale, and no other model has been proposed for larger scales. The scale dependence of runoff and infiltration is currently explained by the spatial and temporal variability of precipitations, soil properties, vegetation and topography. Only soil properties spatial variability is considered here. We investigate in a stochastic framework the rainfall partitioning on slopes with random infiltrabilities by means of theoretical developments and numerical simulations. We consider a variation of infiltrability IM along a 1D slope, under a constant rainfall intensity R of uniform repartition. The infiltration function I is defined either by an Horton law, where I(R)=R if R