Possession Sound is a dynamic salt wedge estuary system near Everett, Washington that is fed by the Snohomish River. In salt wedge estuaries, a mix of salt and fresh water creates a salinity gradient between the two sources, with the denser, saltier water making up the lower sections of the vertical gradient, and the freshwater residing above it. Turbulence from river flow and tidal currents decreases the concentration of suspended sediment in the water column, measured as turbidity. As stratification increases, turbulence increases too, which then causes lower turbidity. This study explores influences on turbidity at the Everett Marina during the year 2020. In the Everett Marina, North flow corresponds with flood tides, and South flow during ebb tides. During these tidal exchanges, the prediction is that when the tide is slack, the horizontal velocities of the water would show an east/west flow. This east/west flow would create vertical mixing because of upwelling and higher turbidity in the water. Two-dimensional horizontal river flow velocities from 0.9 to 4.9 meters from the riverbed at half-meter and meter increments were measured using a grant-supported deployment of an Aquadopp ADCP (Acoustic Doppler Current Profiler). Turbidity was collected using a CTD deployed 1.7 meters from the surface. The volume, velocity, and sediment deposition of river water were compiled from the United States Geological Survey (USGS), and tide heights were published by the National Oceanic and Atmospheric Administration (NOAA). Preliminary results indicate an inverse relationship between tidal height and turbidity and with an emphasis on further Spatio-temporal relationships, more conclusions may be found. The Everett Marina hosts dredging of the estuary in order to maintain safe river flow to the Possession sound itself. Without this river flow, needed nutrients may not reach the saltwater, disrupting the ecosystem, and increasing flooding.