Estuarine and Coastal Hydrography and Sediment Transport 2017
DOI: 10.1017/9781139644426.010
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Sediment Transport: Instrumentation and Methodologies

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(2 citation statements)
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“…Point measurements of wind speed and proxies of sediment fluxes are often collected to derive/validate relationships between sediment fluxes and the local wind speed (e.g., Davidson‐Arnott et al., 2005; de Vries et al., 2014; Hoonhout & de Vries, 2017). However, wind speed and sediment transport measured with point measurement methods such as cup, vane, or sonic anemometers and sediment traps, saltiphones, or laser sensors, respectively, only give an indication of transport at one location (Black et al., 2017; van Rijn, 2019; White, 1998). They do not provide information on the spatial patterns of wind speed or sediment particle transport.…”
Section: Introductionmentioning
confidence: 99%
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“…Point measurements of wind speed and proxies of sediment fluxes are often collected to derive/validate relationships between sediment fluxes and the local wind speed (e.g., Davidson‐Arnott et al., 2005; de Vries et al., 2014; Hoonhout & de Vries, 2017). However, wind speed and sediment transport measured with point measurement methods such as cup, vane, or sonic anemometers and sediment traps, saltiphones, or laser sensors, respectively, only give an indication of transport at one location (Black et al., 2017; van Rijn, 2019; White, 1998). They do not provide information on the spatial patterns of wind speed or sediment particle transport.…”
Section: Introductionmentioning
confidence: 99%
“…Ripples primarily transport sediment in the form of creep (Sharp, 1963). The creep transport rates associated with ripple migration have been related to the total sediment transport rates (Sherman et al, 2019) indication of transport at one location (Black et al, 2017;van Rijn, 2019;White, 1998). They do not provide information on the spatial patterns of wind speed or sediment particle transport.…”
Section: Introductionmentioning
confidence: 99%