Приказ основних података о документу

dc.creatorPearce, Sophie
dc.creatorLjubičić, Robert
dc.creatorPeña-Haro, Salvador
dc.creatorPerks, Matthew
dc.creatorTauro, Flavia
dc.creatorPizarro, Alonso
dc.creatorDal Sasso, Silvano
dc.creatorStrelnikova, Dariia
dc.creatorGrimaldi, Salvatore
dc.creatorMaddock, Ian
dc.creatorPaulus, Gernot
dc.creatorPlavšić, Jasna
dc.creatorProdanović, Dušan
dc.creatorManfreda, Salvatore
dc.date.accessioned2020-04-04T17:46:33Z
dc.date.available2020-04-04T17:46:33Z
dc.date.issued2020
dc.identifier.issn2072-4292
dc.identifier.urihttps://grafar.grf.bg.ac.rs/handle/123456789/1869
dc.description.abstractImage velocimetry has proven to be a promising technique for monitoring river flows using remotely operated platforms such as Unmanned Aerial Systems (UAS). However, the application of various image velocimetry algorithms has not been extensively assessed. Therefore, a sensitivity analysis has been conducted on five different image velocimetry algorithms including Large Scale Particle Image Velocimetry (LSPIV), Large-Scale Particle Tracking Velocimetry (LSPTV), Kanade–Lucas Tomasi Image Velocimetry (KLT-IV or KLT), Optical Tracking Velocimetry (OTV) and Surface Structure Image Velocimetry (SSIV), during low river flow conditions (average surface velocities of 0.12–0.14 m s−1, Q60) on the River Kolubara, Central Serbia. A DJI Phantom 4 Pro UAS was used to collect two 30-second videos of the surface flow. Artificial seeding material was distributed homogeneously across the rivers surface, to enhance the conditions for image velocimetry techniques. The sensitivity analysis was performed on comparable parameters between the different algorithms, including the particle identification area parameters (such as Interrogation Area (LSPIV, LSPTV and SSIV), Block Size (KLT-IV) and Trajectory Length (OTV)) and the feature extraction rate. Results highlighted that KLT and SSIV were sensitive to changing the feature extraction rate; however, changing the particle identification area did not affect the surface velocity results significantly. OTV and LSPTV, on the other hand, highlighted that changing the particle identification area presented higher variability in the results, while changing the feature extraction rate did not affect the surface velocity outputs. LSPIV proved to be sensitive to changing both the feature extraction rate and the particle identification area. This analysis has led to the conclusions that for surface velocities of approximately 0.12 m s−1 image velocimetry techniques can provide results comparable to traditional techniques such as ADCPs. However, LSPIV, LSPTV and OTV require additional effort for calibration and selecting the appropriate parameters when compared to KLT-IV and SSIV. Despite the varying levels of sensitivity of each algorithm to changing parameters, all configuration image velocimetry algorithms provided results that were within 0.05 m s−1 of the ADCP measurements, on average.en
dc.language.isoensr
dc.publisherMDPIsr
dc.relationCOST Action CA16219 “HARMONIOUS—Harmonization of UAS techniques for agricultural and natural ecosystems monitoring”sr
dc.relationinfo:eu-repo/grantAgreement/MESTD/Technological Development (TD or TR)/37010/RS//
dc.relationinfo:eu-repo/grantAgreement/MESTD/Technological Development (TD or TR)/37009/RS//
dc.rightsopenAccesssr
dc.sourceRemote Sensingsr
dc.subjectimage velocimetrysr
dc.subjectUASsr
dc.subjectriver flow monitoringsr
dc.subjectLSPIVsr
dc.subjectLSPTVsr
dc.subjectKLTsr
dc.subjectOTVsr
dc.subjectSSIVsr
dc.subjectsurface flow velocitysr
dc.titleAn Evaluation of Image Velocimetry Techniques under Low Flow Conditions and High Seeding Densities Using Unmanned Aerial Systemsen
dc.typearticlesr
dc.rights.licenseARRsr
dc.citation.issue2
dc.citation.rankM21~
dc.citation.volume12
dc.identifier.doi10.3390/rs12020232
dc.identifier.fulltexthttps://grafar.grf.bg.ac.rs/bitstream/id/7130/bitstream_7130.pdf
dc.identifier.scopus2-s2.0-85081082127
dc.identifier.wos000515569800031
dc.type.versionpublishedVersionsr


Документи

Thumbnail

Овај документ се појављује у следећим колекцијама

Приказ основних података о документу