000146729 001__ 146729
000146729 005__ 20180913055658.0
000146729 0247_ $$2doi$$a10.1029/2009WR008190
000146729 037__ $$aARTICLE
000146729 245__ $$aOn the influence of gravel bed dynamics on velocity power spectra
000146729 269__ $$a2010
000146729 260__ $$c2010
000146729 336__ $$aJournal Articles
000146729 520__ $$aA series of flume experiments were conducted to study the effect of bed form dynamics on the flow over a gravel bed comprising a wide distribution of grain sizes. Instantaneous high-frequency streamwise flow velocities were sampled using an acoustic Doppler velocimeter at a frequency of 200 Hz, while the simultaneous bed elevations were sampled using sonar transducers at a frequency of 0.2 Hz for a duration of 20 h. Spectral analysis of the measured velocity fluctuations reveals the existence of two distinct power law scaling regimes. At high frequencies, an inertial subrange of turbulence with ∼−5/3 Kolmogorov scaling is observed. At low frequencies, another scaling regime with spectral slope of about −1.1 is found. We interpret this range as the signature of the evolving multiscale bed topography on the near-bed velocity fluctuations. The two scaling ranges are separated by a spectral gap, i.e., a range of intermediate scales with no additional energy contribution. The high-frequency limit of the spectral gap corresponds to the integral scale of turbulence. The low-frequency end of the gap corresponds to the scale of the smallest bed forms identified by the velocity sensor, which depends on the position of the sensor. Our results also show that the temporal scales of the largest bed forms can be potentially identified from spectral analysis of low-resolution velocity measurements collected near the channel bed. 
000146729 700__ $$aSingh, A.
000146729 700__ $$0243661$$aPorté-Agel, F.$$g168244
000146729 700__ $$aFoufoula-Georgiou, E.
000146729 773__ $$j46$$qW04509$$tWATER RESOURCES RESEARCH
000146729 909C0 $$0252260$$pWIRE$$xU12172
000146729 909CO $$ooai:infoscience.tind.io:146729$$particle$$pENAC
000146729 917Z8 $$x173008
000146729 937__ $$aWIRE-ARTICLE-2010-030
000146729 973__ $$aOTHER$$rREVIEWED$$sPUBLISHED
000146729 980__ $$aARTICLE