论文部分内容阅读
A 3-D baroclinic numerical model is established to study the temporal and spatial distribution of salinity in the North Branch (NB) of the Yangtze Estuary (YE) in response to river runoff, wind and currents. The idealized, process-oriented studies show that the lower river runoff in the dry season is the main driving factor for the spilling over from the NB to the South Branch (SB). The NB takes longer time to get in dynamic stable state compared with the SB, as the runoff transfers from the wet season to the dry season. The vertical stratification intensity of the NB has obvious periodic phenomena in the dry season, and the stratification strength is enhanced under the action of low runoff and north wind, which further weakens the vertical transport of water. Momentum balance analysis suggested that the landward net flux increases when considering the influence of the moderate north wind, and the landward flux will enhance if considering the boundary current during the spring tide. With the influence of the boundary current, increases the average salinity of the NB, as well as the intrusion degree from the NB to the SB. This indicates that the nearshore ocean current of the Yellow Sea is an important factor affecting the saltwater intrusion in the NB of the YE.