Variability of particle characteristics in a wave- and current-driven estuarine environment

Grace Chang1, Galen Egan2, Frank Spada1, Craig Alexander Jones1, Andrew J Manning3, Stephen G Monismith4 and Oliver B Fringer5, (1)Integral Consulting Inc., Santa Cruz, CA, United States, (2)Sofar Ocean, San Francisco, United States, (3)University of Hull, Hull, United Kingdom, (4)Stanford University, Stanford, California, United States, (5)Stanford University, Stanford, CA, United States
Abstract:
We deployed in-situ acoustical and optical instrument platforms to measure the flow and physio-biogeochemical characteristics of sediment at multiple depths above the sediment bed in a turbulent, wave- and current-driven shallow estuarine environment. High resolution acoustic Doppler velocimeters provided information with which to understand physical forcing processes. Optical sensors (Laser In-Situ Scattering and Transmissometry (LISST), spectral absorption and attenuation meters, optical backscattering meters, chlorophyll fluorometers, and a Sediment Profile Imaging camera) enabled determination of particle characteristics (concentration, size distribution, and composition) from time scales ranging from minutes to months. Results show that in different flow environments, short-term (minutes to hours) physical forcing acted to resuspend relatively dense, inorganic particles as well as disaggregate less dense, organic flocculates. Particle processes were primarily dependent on wind-driven, wave-induced physical forcing and seasonal biogeochemical variability. The suite of data obtained from the field observations will inform a high-resolution large-eddy simulation model to understand the relationship between particle size distributions and turbulence in wave-driven estuarine environments and how these dynamics affect and are affected by time scales of biogeochemical properties of the suspended particles.