Inferring sediment transfers and functional connectivity of rivers from repeat topographic surveys (supporting information)

dc.contributor.authorCalle, Mikel
dc.contributor.authorCalle, Javier
dc.contributor.authorAlho, Petteri
dc.contributor.authorBenito, Gerardo
dc.coverage.spatialeast=-0.14227852370471084; north=40.105520380219254; name=4V45+63 Costur, España
dc.data.typeConjunto de datos
dc.date.accessioned2026-03-03T16:17:11Z
dc.date.available2026-03-03T16:17:11Z
dc.date.issued2020-01-13
dc.descriptionInformación suplementaria asociada a la publicación y ejemplos de datos de entrada y de salida
dc.description.abstractHigh-resolution topographic models have revolutionized monitoring of river changes by comparing sequential river topographic surveys (i.e. change detection). Nevertheless, much more may be obtained from this innovative quantification of changes. In this paper, we enhance the interpretation of geomorphic processes by presenting a new method for understanding of sources and sinks of sediment, river sediment transfers and functional sediment connectivity. Repeat digital elevation models (DEMs) obtained by photogrammetry were used to quantify topographic change after two floods by creating a DEM of difference (DoD) of a 6.5 km-long reach of Rambla de la Viuda stream, an ephemeral gravel-bed river in eastern Spain. The proposed method involved dividing the channel into 10 m-long longitudinal strips that were used to systematically draw boundaries between the erosional and depositional areas of the DoD. The analysis objectively: (i) drew a series of erosional and depositional segments, from 120 to 1360 m in length; (ii) estimated ranges of source-to-storage sediment transport distances, 320–670 m in the upstream and middle reaches and up to 2030 m in the lower reach; and (iii) obtained values of functional connectivity (i.e. the ratio between the sediment exported (erosion) and retained (deposition), ranging from 103 to 10−3). The variability in these three parameters along the river was found to be related to the level of channel disturbance by in-stream mining during the 1990s and 2000s. Additionally, this method indicates that the main process responsible for self-adjustment of the present morphosedimentary conditions is intra-reach erosion of banks and channel beds. Thus, this study proposes a new methodology to characterize morphological change, sediment transfer and connectivity that may serve as environmental indicators of the hydromorphological integrity of rivers with potential application to the European Water Framework Directive.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.sponsorshipMinisterio de Economía y Competitividad
dc.description.sponsorshipAcademy of Finland
dc.description.statuspub
dc.identifier.doi10.1002/esp.4765
dc.identifier.issn0197-9337
dc.identifier.issn1096-9837
dc.identifier.officialurlhttps://onlinelibrary.wiley.com/doi/10.1002/esp.4765
dc.identifier.urihttps://hdl.handle.net/20.500.14352/133744
dc.language.isoeng
dc.publisherWiley
dc.relation.projectIDCGL2014-58127-C3-1-R
dc.relation.projectIDCGL2017-86839-C3-1-R
dc.relation.projectIDBES-2012-056723
dc.relation.projectIDGrant 293389
dc.rightsAttribution-NonCommercial 4.0 Internationalen
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/
dc.subject.cdu551.312.3
dc.subject.keywordFunctional connectivity
dc.subject.keywordChange detection
dc.subject.keywordSfM-MVS
dc.subject.keywordTransport distance
dc.subject.keywordHydromorphological assessment
dc.subject.ucmHidrología
dc.subject.unesco2506.07 Geomorfología
dc.titleInferring sediment transfers and functional connectivity of rivers from repeat topographic surveys (supporting information)
dc.typedataset
dc.type.hasVersionVoR
dspace.entity.typePublication

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