“…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.…”