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首页> 外文期刊>Ocean & coastal management >Importance of large-scale coastal circulation on bay-shelf exchange and residence time in a subtropical embayment, the northern South China Sea
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Importance of large-scale coastal circulation on bay-shelf exchange and residence time in a subtropical embayment, the northern South China Sea

机译:南海北部副热带海域大规模海岸环流对海湾-陆架交换和停留时间的重要性

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摘要

A nested ocean model with a particle tracking module is used to investigate the bay-shelf exchange and the residence time in Daya Bay (DB) in the northern South China Sea in the presence of coastal circulation with a prominent seasonal cycle. The model reasonably reproduces the key features of the seasonal mean circulation in DB and its adjacent coastal waters. The summertime longitudinal circulation is characterized by a two-layer structure, with a surface seaward flow above a landward, slope-climbing flow at the bottom. In winter, however, it is characterized by a vertically well-mixed, cyclonic, lateral circulation, with a landward (seaward) flow on the eastern (western) flank. Therefore, the residence time in the upper layer of DB is much shorter during summer than winter. Numerical experiments were conducted to quantify the relative roles of the large-scale coastal circulation and other processes (e.g., local winds, tides, river and cooling water discharge) on the residence time. The large-scale coastal circulation and the local winds are the main drivers of the upper-layer residence time. The large-scale coastal circulation controlled the seasonal pattern of bay-shelf exchange and the residence time in DB, whereas the local wind effect was comparable with the large-scale coastal circulation and had a greater effect in winter. The local wind reduces residence time by intensifying the upwelling (downwelling) circulation and has substantial effects on the spatial distribution of the residence time within DB. In addition to the large-scale coastal circulation and local wind, the residence time is regulated by tides, river and cooling water discharge. Moreover, during the extreme weather conditions (e.g., tropical storm and typhoon), the residence time is significantly reduced by the intensified bay-shelf exchange. The spatial and temporal variation of residence time in DB is of great significance in the regional coastal management for marine environmental protection.
机译:使用带有粒子跟踪模块的嵌套海洋模型,研究在存在明显季节性周期的沿海环流的情况下,南海北部大亚湾(DB)的海湾-陆架交换和停留时间。该模型合理地再现了DB及其附近沿海水域的季节性平均环流的关键特征。夏季的纵向环流具有两层结构,地表海流在陆上的上方,底部是斜坡。然而,在冬季,它的特点是垂直混合均匀,气旋,侧向循环,东部(西部)侧面有陆运(向海)流动。因此,夏季在DB上层的停留时间比冬季短得多。进行了数值实验,以量化大规模沿海环流和其他过程(例如局部风,潮汐,河流和冷却水排放)对停留时间的相对作用。大规模的沿海环流和局部风是上层停留时间的主要驱动力。大规模的沿海环流控制着海湾-陆架交换的季节模式和在DB中的停留时间,而局部风效应可与大规模的沿海环流相媲美,并且在冬季影响更大。局部风通过增强上升流(下降流)的循环来减少停留时间,并且对DB内停留时间的空间分布有重大影响。除了大规模的沿海环流和局部风以外,滞留时间还受到潮汐,河流和冷却水排放的限制。此外,在极端天气条件下(例如,热带风暴和台风),通过密集的海湾-架子交换大大缩短了停留时间。 DB中停留时间的时空变化对海洋环境保护的区域沿海管理具有重要意义。

著录项

  • 来源
    《Ocean & coastal management》 |2019年第2期|72-89|共18页
  • 作者单位

    Sun Yat Sen Univ, Sch Marine Sci, Guangzhou 510275, Guangdong, Peoples R China|Sun Yat Sen Univ, Guangdong Prov Key Lab Marine Resources & Coastal, Guangzhou 510275, Guangdong, Peoples R China|Sun Yat Sen Univ, Guangdong Prov Key Lab Climate Change & Nat Disas, Guangzhou 510275, Guangdong, Peoples R China;

    Sun Yat Sen Univ, Sch Marine Sci, Guangzhou 510275, Guangdong, Peoples R China;

    Sun Yat Sen Univ, Sch Marine Sci, Guangzhou 510275, Guangdong, Peoples R China;

    Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China;

    Sun Yat Sen Univ, Sch Marine Sci, Guangzhou 510275, Guangdong, Peoples R China|Sun Yat Sen Univ, Guangdong Prov Key Lab Marine Resources & Coastal, Guangzhou 510275, Guangdong, Peoples R China;

    Sun Yat Sen Univ, Sch Marine Sci, Guangzhou 510275, Guangdong, Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Large-scale coastal circulation; Residence time; Nested Ocean model; Daya bay; Northern South China Sea;

    机译:大规模沿海环流;停留时间;巢海模式;大亚湾;南海北部;

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