Please login to be able to save your searches and receive alerts for new content matching your search criteria.
Field observations of the currents at a bending channel in the Abashiri River in Hokkaido, Japan have revealed an unexpected secondary circulation during flood tide with near-bed and near-surface currents toward the outer and inner banks of the bend, respectively. The direction of these cross-stream currents was reversed at the end of flood tide. The occurrence and shutdown of these observed unexpected secondary circulation were further investigated through the shape of the along-channel velocity profile by using a theoretical solution based on the steady-state momentum equation and the Stokes’s second problem for oscillating flow. Also, an advanced numerical model was used to quantify the unexpected secondary flow. It was shown from the theoretical analysis that vertical advection plays a great role in the momentum balance affecting the direction of secondary flows. The typical secondary flow was found to occur throughout ebb tide with a pronounced near-surface maximum velocity profile. Whereas, during flood tide, the longitudinal velocity profile was characterized by a near-bed and mid-depth maximum, resulting an upwelling flow near the outer bank. These findings were reconfirmed by numerical simulations that were conducted for the entire estuary.
The effects of hydrodynamic and mixing conditions on the variation of phytoplankton composition and their habitats were investigated in the tide-dominated macrotidal Chikugo River estuary during a neap-spring tidal cycle in 2021. The estuary changed from stratified to well-mixed conditions during a neap-spring transition. The river discharge was < 60 m3s-1 during the study period. Seawater intruded towards 17 km (upstream) during neap tide and until 16 km during spring tide. Surface suspended sediment concentration (SSC) was low during neap tide and maximum (∼400 mg/L) during spring tide corresponding with changes in mixing and an estuarine turbidity maximum (ETM) was developed between 8-12 km during spring tide. Marine habitats diatoms were the major group with 20-89% of total phytoplankton. During a neap-spring tidal cycle, the maximum abundance of freshwater green algae was found during neap tide while diatoms (both marine and freshwater habitats) was in two days after neap tide and freshwater blue-green algae was in intermediate tide in response to changes in mixing conditions. The distribution of marine habitat diatoms and freshwater blue-green algae were positively correlated with salinity whereas freshwater green algae and freshwater habitat diatoms were negatively correlated with salinity. This study concludes that saltwater intrusion and mixing conditions driven by tidal forcing mainly controlled the species composition and their habitats in the Chikugo River estuary.