... sea area. The influence of the wind and tide conditions were also analyzed. The results showed that the particles reached to the observation points faster during the ebb tide than the flood tide. The diffusion area of the oil spill was also larger during the flood tide. Under the condition of calm...

... by the reclamation and suspended sediment transport process due to dredging over the intertidal flat, where the tidal current due to local force tide rather than small wave is the dominant dynamic for sediment transport and morphology. A two-dimensional numerical model discretized by a cell-centered finite volume...

... Abstract Hydrodynamics and suspended sediment concentration of tide-induced bottom boundary layer have been observed by a self-designed measuring system during August 8-10, 2013 at intertidal flats in the central part of Jiangsu coast. An advanced Acoustic Doppler Velocity Profiler "Vectrino...

... Abstract Harmonic analysis was carried out on tide data of Lianxinggang and Qinglonggang station, which are located in the downstream and upstream of the north branch of the Yangtze Estuary, respectively. Some appropriate parameters are selected to characterize the geomorphology features...

... Abstract This paper investigates the effects of potential future 1m sea level rise (SLR) on the tides in the Pearl River Estuary (PRE) using a validated 2D tidal model based on MIKE21. The results of 1 m SLR scenario indicate that 1) the co-change lines of amplitude and phase are approximately...

... ABSTRACT: When tides flow over the ocean floor, they exert dynamic pressure on the porous seabed, and consequently result in oscillatory pore pressure and seepage in the seabed. Stability of the large-diameter pipelines under construction immersed in the seabed may be influenced by the excess...

..., the main ebb tide direction near the Qiqu Archipelago is about 110 degree, flood tide direction is about 280 degree; ebb tide direction between Dayangshan and Xiaoyangshan is about 120 degree while flood tide direction is about 290 degree, and tide here has strong reciprocation characteristic. Water flow...

... Breeding The tide during asari clam breeding (larva generation) greatly changes not only in terms of the sea area where the larvae can reach, but also the number of larvae surviving in the bay. This is considered to change greatly the existence and situation of the asari clam network in the bay. In Tokyo...

... intensive in all layers. The tidal change is very complex, there is tide in someplace,while no tide in other place;the tidal range varies from 4m to 0.5m. In addition to regular astronomical tide, there is storm tide which is difficul t to be predicted. When the storm tide comes, the sea can intrude ashore...