2014
DOI: 10.1016/j.advwatres.2014.04.004
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Capabilities of Large-scale Particle Image Velocimetry to characterize shallow free-surface flows

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Cited by 64 publications
(45 citation statements)
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“…Large‐scale particle image velocimetry, for example, has been developed for fast and effective discharge estimation of floods, where conventional, intrusive equipment can no longer be used (see, e.g., Muste, Fujita, & Hauet, ). However, it has been reported that more complex, transient flow features can also be investigated with this method (Muste et al, ). Studies have shown that large‐scale particle image velocimetry can also be used to quantify, for example, surface velocities in the proximity of breaking waves and the associated run‐up, as the generated foam is an adequate tracer for the algorithm (e.g., Fleit et al, ; Fleit & Baranya, ).…”
Section: Discussionmentioning
confidence: 99%
“…Large‐scale particle image velocimetry, for example, has been developed for fast and effective discharge estimation of floods, where conventional, intrusive equipment can no longer be used (see, e.g., Muste, Fujita, & Hauet, ). However, it has been reported that more complex, transient flow features can also be investigated with this method (Muste et al, ). Studies have shown that large‐scale particle image velocimetry can also be used to quantify, for example, surface velocities in the proximity of breaking waves and the associated run‐up, as the generated foam is an adequate tracer for the algorithm (e.g., Fleit et al, ; Fleit & Baranya, ).…”
Section: Discussionmentioning
confidence: 99%
“…In the light of such a present status of discharge measurement, the so-called non-intrusive measurement techniques have been paid attention to in recent years, such as a radio-wave velocity meter (RVM) [6,7] or imaging techniques [8][9][10][11][12]. The RVM is usually installed at a bridge to measure streamwise surface velocity continuously at one point by using the effect of the Doppler shift of the surface flow [6,7].…”
Section: Introductionmentioning
confidence: 99%
“…The fact that the MAPE of 9.00% is considerably below the variability of the discharges among multiple profiles (see section 4.4) indicates that the spatiotemporal averaging of multiple profiles is indeed effective to account for a large part of random errors that might result from local errors in the DTMs, water masks or flow velocities. Overall the residual errors are very similar to results from previous LSPIV studies at various sites [ Muste et al ., ].…”
Section: Resultsmentioning
confidence: 99%