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A multi-resolution method to map and identify locations of future gully and channel incision

dc.contributor.authorWalker, Simon
dc.contributor.authorWilkinson, Scott N.
dc.contributor.authorVan Dijk, Albert
dc.contributor.authorHairsine, Peter
dc.date.accessioned2020-07-14T05:26:13Z
dc.date.issued2020-02-28
dc.date.updated2020-03-23T21:44:51Z
dc.description.abstractWhile channel erosion is recognised as a major, often-dominant, source of river sediment, channel geometry and its change remain impractical to measure for anything but small experimental watersheds. Designing remediation strategies in landscapes affected by channel erosion requires information on the extent and location of current incised channel features, as well as a method to determine locations where incision may occur in the future. We present a multi-resolution algorithm that uses topographic information to concurrently map both existing incised landform elements and areas at risk of future incision. The former uses elevation, slope and profile curvature to identify topographic signatures of incised landform elements, and the latter uses landscape position, topographic wetness index and stream power index to isolate areas likely susceptible to future incision. We aimed to develop a computationally efficient method capable of operating across a broad range of landscapes. The algorithm was tested in three contrasting environments in eastern Australia with promising results. Sensitivity analysis indicates the method performs reasonably consistently across landscapes, but that outputs become more sensitive as the average slope of the landscape increases. A comparison between cleared and uncleared hillsides suggested that areas indicated at risk of future incision are plausible, and that cleared areas were more susceptible to channel incision. The only required input is a digital elevation model, and outputs can provide a rapid visual assessment of landscapes affected by incisional erosion. This technique enables the identification of gully erosion and the planning of remediation works across landscapes of thousands of square kilometres. It may assist in prioritisation of works and further insights into the processes associated with channel incision.en_AU
dc.description.sponsorshipFunding for this research was supported by the Commonwealth Scientific and Industrial Research Organisation (CSIRO) and also by the Australian Government's National Environment Science Program (NESP) Tropical Water Quality Hub (Projects 2.1.4 and 5.9). Simon Walker also receives a scholarship under the Australian Government Research Training Program (AGRTP) to support his PhD program.en_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn0169-555Xen_AU
dc.identifier.urihttp://hdl.handle.net/1885/206154
dc.language.isoen_AUen_AU
dc.publisherElsevieren_AU
dc.rights© 2020 Crownen_AU
dc.sourceGeomorphologyen_AU
dc.subjectGully Erosionen_AU
dc.subjectDigital Elevation Modelen_AU
dc.subjectMulti-Resolution Algorithmen_AU
dc.subjectLiDARen_AU
dc.titleA multi-resolution method to map and identify locations of future gully and channel incisionen_AU
dc.typeJournal articleen_AU
dcterms.dateAccepted2020-02-21
local.bibliographicCitation.lastpage16en_AU
local.bibliographicCitation.startpage1en_AU
local.contributor.affiliationWalker, Simon, College of Science, ANUen_AU
local.contributor.affiliationWilkinson, Scott N, CSIRO Land and Wateren_AU
local.contributor.affiliationVan Dijk, Albert, College of Science, ANUen_AU
local.contributor.affiliationHairsine, Peter, College of Science, ANUen_AU
local.contributor.authoruidWalker, Simon, u4475125en_AU
local.contributor.authoruidVan Dijk, Albert, u5250651en_AU
local.contributor.authoruidHairsine, Peter, u5681857en_AU
local.description.embargo2037-12-31
local.description.notesImported from ARIESen_AU
local.identifier.absfor040601 - Geomorphology and Regolith and Landscape Evolutionen_AU
local.identifier.absseo961202 - Rehabilitation of Degraded Farmland, Arable Cropland and Permanent Cropland Environmentsen_AU
local.identifier.ariespublicationu1055894xPUB230en_AU
local.identifier.citationvolume358en_AU
local.identifier.doi10.1016/j.geomorph.2020.107115en_AU
local.type.statusPublished Versionen_AU

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