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LOW-SALINITY PLUME IN THE CHANGJIANG AND ADJACENT COASTAL REGIONS: A MODEL-DATA COMPARISON

机译:低盐度羽流在长江和邻近的沿海地区:模型 - 数据比较

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A three-dimensional (3-D) unstructured-grid, free-surface, primitive equation, Finite-Volume Coastal Ocean Model (FVCOM) was applied to simulate the temporal and spatial structures of the Changjiang plume and examine the process of tidal mixing via river discharge. FVCOM is robust to reproduce the vertical and horizontal variations of the water salinity within the plume area and frontal zone that were observed in the 2005 summertime field survey. The process-oriented studies clearly show that the Changjiang plume is characterized mainly by a two-layer dynamics system with significant influence from local complex bathymetry. A high-resolution model with capability of resolving irregular coastal geometry and rapidly change bottom topography is required to capture the reality of the Changjiang plume.
机译:三维(3-D)非结构化网,自由表面,原始方程,有限体积的沿海海洋模型(FVCOM)应用于模拟长江羽流的时间和空间结构,并检查潮汐混合过程的过程河流排放。 FVCOM具有稳健的是,在2005夏季夏季调查中繁殖的羽流区域和前部区域的垂直和水平变化再现。以过程为导向的研究表明,长江羽流主要是由两层动力学系统的特征在于局部复杂碱基碱的两层动力学系统。需要解决不规则沿海几何和快速改变底部地形的能力的高分辨率模型,以捕捉长江羽流的现实。

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