Amirshahi, Seyed Mohammad; Kwoll, Eva; Winter, Christian (2018): Acoustic doppler velocimeter (ADV) measurements and suspended sediment concentration at station HE441/07-1 in the German Bight. PANGAEA, https://doi.org/10.1594/PANGAEA.889958, Supplement to: Amirshahi, SM et al. (2018): Near bed suspended sediment flux by single turbulent events. Continental Shelf Research, 152, 76-86, https://doi.org/10.1016/j.csr.2017.11.005
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The role of small scale single turbulent events in the vertical mixing of near bed suspended sediments was explored in a shallow shelf sea environment. High frequency velocity and suspended sediment concentration (SSC; calibrated from the backscatter intensity) were collected using an Acoustic Doppler Velocimeter (ADV). Using quadrant analysis, the despiked velocity time series was divided into turbulent events and small background fluctuations. Reynolds stress and Turbulent Kinetic Energy (TKE) calculated from all velocity samples, were compared to the same turbulent statistics calculated only from velocity samples classified as turbulent events (Re_events and TKE_events). The comparison showed that Re_events and TKE_events was increased 3 and 1.6 times, respectively, when small background fluctuations were removed and that the correlation with SSC for TKE could be improved through removal of the latter. The correlation between instantaneous vertical turbulent flux (w') and SSC fluctuations (SSC') exhibits a tidal pattern with the maximum correlation at peak ebb and flood currents, when strong turbulent events appear. Individual turbulent events were characterized by type, strength, duration and length. Cumulative vertical turbulent sediment fluxes and average SSC associated with individual turbulent events were calculated. Over the tidal cycle, ejections and sweeps were the most dominant events, transporting 50% and 36% of the cumulative vertical turbulent event sediment flux, respectively. Although the contribution of outward interactions to the vertical turbulent event sediment flux was low (11%), single outward interaction events were capable of inducing similar SSC' as sweep events. The results suggest that on time scales of tens of minutes to hours, TKE may be appropriate to quantify turbulence in sediment transport studies, but that event characteristics, particular the upward turbulent flux need to be accounted for when considering sediment transport on process time scales.
Median Latitude: 54.091302 * Median Longitude: 7.358536 * South-bound Latitude: 54.091170 * West-bound Longitude: 7.358000 * North-bound Latitude: 54.091830 * East-bound Longitude: 7.358670
Date/Time Start: 2015-03-21T00:12:00 * Date/Time End: 2015-03-21T12:41:59
Datasets listed in this publication series
- Amirshahi, SM; Kwoll, E; Winter, C (2018): Instantaneous suspended sediment concentration (SSC) from ADV 12 cm above seabed at station HE441/07-1 in the German Bight. https://doi.org/10.1594/PANGAEA.889952
- Amirshahi, SM; Kwoll, E; Winter, C (2018): Instantaneous flow velocity magnitude (V) from ADV 12 cm above seabed at station HE441/07-1 in the German Bight. https://doi.org/10.1594/PANGAEA.889949
- Amirshahi, SM; Kwoll, E; Winter, C (2018): Instantaneous flow velocity in the streamwise direction (Vx) from ADV 12 cm above seabed at station HE441/07-1 in the German Bight. https://doi.org/10.1594/PANGAEA.889919
- Amirshahi, SM; Kwoll, E; Winter, C (2018): Instantaneous flow velocity in the crossstream direction (Vy) from ADV 12 cm above seabed at station HE441/07-1 in the German Bight. https://doi.org/10.1594/PANGAEA.889842
- Amirshahi, SM; Kwoll, E; Winter, C (2018): Instantaneous flow velocity in the vertical direction (Vz) from ADV 12 cm above seabed at station HE441/07-1 in the German Bight. https://doi.org/10.1594/PANGAEA.889946