Comparison of remote sensing based approaches for mapping bathymetry of shallow, clear water rivers

dc.contributor.authorE. Kasvi
dc.contributor.authorJ. Salmela
dc.contributor.authorE. Lotsari
dc.contributor.authorT. Kumpula
dc.contributor.authorS.N. Lane
dc.contributor.organizationfi=maantiede|en=Geography |
dc.contributor.organizationfi=maantieteen ja geologian laitos|en=Department of Geography and Geology|
dc.contributor.organization-code1.2.246.10.2458963.20.17647764921
dc.contributor.organization-code1.2.246.10.2458963.20.23186815876
dc.contributor.organization-code2606901
dc.converis.publication-id39717375
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/39717375
dc.date.accessioned2022-10-27T11:55:02Z
dc.date.available2022-10-27T11:55:02Z
dc.description.abstract<p>Shallow rivers provide important habitat for various aquatic and terrestrial species. The bathymetry of such environments is, however, difficult to measure as devices and approaches have been traditionally developedmainly for deeper waters. This study addresses the mapping of shallow water bathymetry with high spatial resolution and accuracy by comparing three remote sensing (RS) approaches: one based on echo sounding (active RS) and two on photogrammetry (passive RS): bathymetric Structure from Motion (SfM) and optical modelling. The tests were conducted on a 500 m long and ~30 m wide reach of sand bedded meandering river: (1) during a rising spring flood (Q=10–15m3/s)withmediumturbidity and highwater color and; (2) during autumn low discharge (Q =4 m3/s) with low turbidity and color. Each method was used to create bathymetric models. The models were compared with high precision field measurements with a mean point spacing of 0.86 m. Echo sounding provided themost accurate (ME~−0.02 m) and precise (SDE=±0.08 m) bathymetricmodels despite the high degree of interpolation needed. However, the echo sounding-based models were spatially restricted to areas deeper than 0.2 m and no small scale bathymetric variability was captured. The quality of the bathymetric SfM was highly sensitive to flow turbidity and color and therefore depth. However, bathymetric SfM suffers less from substrate variability, turbulent flow or large stones and cobbles on the river bed than optical modelling. Color and depth did affect optical model performance, but clearly less than the bathymetric SfM. The optical model accuracy improved in autumn with lower water color and turbidity (ME = −0.05) compared to spring (ME=−0.12). Correlations between the measured and modelled depth values (r=0.96) and the models precision (SDE=0.09–0.11) were close to those achieved with echo sounding. Shadows caused by riparian vegetation restricted the spatial extent of the optical models.<br /></p>
dc.format.pagerange180
dc.format.pagerange197
dc.identifier.eissn1872-695X
dc.identifier.jour-issn0169-555X
dc.identifier.olddbid172794
dc.identifier.oldhandle10024/155888
dc.identifier.urihttps://www.utupub.fi/handle/11111/30643
dc.identifier.urlhttps://doi.org/10.1016/j.geomorph.2019.02.017
dc.identifier.urnURN:NBN:fi-fe2021042821900
dc.language.isoen
dc.okm.affiliatedauthorKasvi, Elina
dc.okm.affiliatedauthorSalmela, Jouni
dc.okm.affiliatedauthorLotsari, Eliisa
dc.okm.discipline1171 Geosciencesen_GB
dc.okm.discipline1171 Geotieteetfi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherElsevier
dc.publisher.countryNetherlandsen_GB
dc.publisher.countryAlankomaatfi_FI
dc.publisher.country-codeNL
dc.relation.doi10.1016/j.geomorph.2019.02.017
dc.relation.ispartofjournalGeomorphology
dc.relation.volume333
dc.source.identifierhttps://www.utupub.fi/handle/10024/155888
dc.titleComparison of remote sensing based approaches for mapping bathymetry of shallow, clear water rivers
dc.year.issued2019

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