Variation in the Current Shear Front and Its Potential Effect on Sediment Transport Over the Inner Shelf of the East China Sea in Winter

• Published in: Journal of geophysical research. Oceans 2018-11, Vol.123 (11), p.8264-8283
• Main Authors: Liu, S. D., Qiao, L. L., Li, G. X., Shi, J. H., Huang, L. L., Yao, Z. G., Gao, F., Wang, Z., Min, J. X.
• Format: Article
• Language: English
• Subjects: Barriers; Channels; Computer simulation; cross‐CSF channels; Current shear; current shear front; Data analysis; Data processing; Direction; Fronts; Geophysics; Hydrodynamics; Identification; inner shelf mud area in the East China Sea; Mathematical analysis; Mathematical models; Mud; Nonuniformity; numerical modeling; Numerical simulations; Salinity; Salinity effects; Sediment; Sediment transport; Shear; Spatial distribution; Spring tides; Suspended sediments; Temperature; Topography; Topography (geology); Transport; Transport processes; Variation; variation mechanism; Wind; Winter
• ISSN: 2169-9275; 2169-9291
• DOI: 10.1029/2018JC014241

The current shear fronts (CSFs) in the East China Sea have been observed during winter in previous studies. In this research, we systematically study characteristics and variation mechanism of the CSFs and its potential effects on the transport of water and suspended sediment and on the inner shelf mud area (ISMA), using the methods of observation data analysis and numerical simulation. The spatial structures, shear intensities, and sea‐land locations of the CSFs are obviously affected by wind, temperature and salinity. The CSFs curve seaward due to the nonuniformity of topography, and the tide causes its periodic and sea‐land shift. The landward U component near the CSFs indicate little cross‐CSF transport (i.e., the barrier effect). The CSFs are important hydrodynamic factors that affect the formation of the ISMA. The periodic shift of the CSFs in the longitudinal direction and its variations in spatial structure are the main mechanisms affecting the spatial distribution and thickness of the ISMA. However, the barrier effect of the CSFs can be interrupted, and both the strong wind in the northeast direction and baroclinic conditions are beneficial for cross‐CSF transport. Furthermore, cross‐CSF transports occur in the upper layers under northwest wind condition, in areas with nonuniformity of topography and during the spring tide period. Three cross‐shelf channels are identified in areas where the CSFs curve seaward resulting from nonuniformity of topography. Plain Language Summary Variation in the current shear front (CSF) and its potential effect on sediment transport over the inner shelf of the East China Sea (ECS) in winter were studied in this paper. Wind, temperature, and salinity affect CSFs in the ECS; topography induces its seaward curve; tide causes its periodic and sea‐land shift. The barrier effect of the CSFs affects the formation of the inner shelf mud area. But three cross‐shelf channels are identified during winter in areas where the CSFs curve seaward resulting from nonuniformity of topography. This study will provide reference for other sea areas where the CSFs have been found and corresponding suspended sediment transport process. Key Points Wind, temperature, salinity, topography, and tide affect current shear fronts in the East China Sea during winter The barrier effect of current shear fronts controls the spatial distribution and thickness of the inner shelf mud area in the East China Sea Three cross‐shelf channels are identified in