Effective timescales of coupling within fluvial systems

• Published in: Geomorphology (Amsterdam) 2002-05, Vol.44 (3), p.175-201
• Main Author: Harvey, Adrian M.
• Format: Article
• Language: English
• Subjects: Alluvial fans; Base level; Bgi / Prodig; Coupling; Earth sciences; Earth, ocean, space; Exact sciences and technology; Fluvial forms and processes; Geomorphology; Gullying; Physical geography; Stratigraphy; Tectonic geomorphology; Tectonics. Structural geology. Plate tectonics
• ISSN: 0169-555X; 1872-695X
• DOI: 10.1016/S0169-555X(01)00174-X

This paper presents a review of the coupling concept in fluvial geomorphology, based mainly on previously published work. Coupling mechanisms link the components of the fluvial system, controlling sediment transport down the system and the propagation of the effects of base-level change up the system. They can be viewed at several scales: at the local scale involving within-hillslope coupling, hillslope-to-channel coupling, and within-channels, tributary junction and reach-to-reach coupling. At larger scales, coupling can be considered as zonal coupling, between major zones of the system or as regional coupling, relating to complete drainage basins. These trends are illustrated particularly by the examples of hillslope-to-channel coupling in the Howgill Fells, northwest England, badland systems in southeast Spain, alluvial fans in Spain, USA and UAE, and base-level-induced dissection of Neogene sedimentary basins in southeast Spain. As the spatial scales increase, so do the timescales involved. Effective temporal scales relate to magnitude and frequency characteristics, recovery time and propagation time, the relative importance changing with the spatial scale. For downsystem coupling at the local scale, the first two are important, with propagation time increasing in importance in larger systems, especially in those involving upsystem coupling related to base-level change. The effective timescales range from the individual event, with a return period of decades, through decadal to century timescales for downsystem coupling, to tens to hundreds of thousands of years for the basinwide response to base-level change. The effective timescales influence the relative importance of factors controlling landform development.