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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Influences of physical processes on the ecosystem in Jiaozhou Bay: A coupled physical and biological model experiment
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Influences of physical processes on the ecosystem in Jiaozhou Bay: A coupled physical and biological model experiment

机译:物理过程对胶州湾生态系统的影响:物理与生物学耦合实验

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In this paper we have used a three-dimensional coupled physical and biological model to examine the marine ecosystem of Jiaozhou Bay. Physical processes included (1) the M_2 tide, (2) river discharges, and (3) winds. The biological model described a simple, phosphorous-based, lower trophic food web system. The model results showed that tidal mixing had a direct impact on temporal and spatial distributions of nutrients and phytoplankton as well as on shellfish aquaculture. Nutrients and phytoplankton were well mixed vertically by tidal motion. Their concentrations were highest around northwestern and northern regions of the bay near river sources and decreased with water depth from the inner bay to the outer bay. A phytoplankton bloom can occur around the northwestern coast due to the "accumulation" of nutrients under southeasterly wind conditions. The flux analysis suggests that in summer the nutrients in Jiaozhou Bay was directly supplied and maintained by physical processes, but the temporal variation of phytoplankton was controlled dominantly by biological processes associated with nutrient uptake, grazing by zooplankton, and consumption by shellfish. Shellfish aquaculture can modify the bay-scale balance of the ecosystem in Jiaozhou Bay. The loss of phytoplankton in shellfish aquaculture sites tended to be compensated by advection and diffusion from the surrounding waters. A large consumption of phytoplankton by shellfish can cause a net flux of phytoplankton from the Yellow Sea to Jiaozhou Bay, although there was a net nutrient flux flowing out of the bay. The physical mechanisms for the water exchange between Jiaozhou Bay and the Yellow Sea was controlled mainly by a chaotic process associated with nonlinear interactions between oscillating tidal currents and double residual eddies.
机译:在本文中,我们使用了三维耦合的物理和生物学模型来研究胶州湾的海洋生态系统。物理过程包括(1)M_2潮,(2)河水排放和(3)风。生物学模型描述了一个简单的,基于磷的低营养食物网系统。模型结果表明,潮汐混合对养分和浮游植物的时空分布以及贝类水产养殖有直接影响。营养物质和浮游植物通过潮汐运动垂直混合均匀。它们的浓度在靠近河源的海湾的西北和北部地区最高,并且随着从内海湾到外海湾的水深而降低。由于东南风条件下养分的“积累”,浮游植物的开花会在西北海岸附近发生。通量分析表明,夏季胶州湾的养分是通过物理过程直接提供和维持的,而浮游植物的时间变化主要受与养分吸收,浮游动物放牧和贝类消费相关的生物过程的控制。贝类养殖可以改变胶州湾生态系统的海湾规模平衡。贝类水产养殖场中浮游植物的损失往往可以通过对流和从周围水域扩散来弥补。贝类对浮游植物的大量消费会导致从黄海到胶州湾的浮游植物净流量,尽管有营养净流量从该海湾流出。胶州湾与黄海之间水交换的物理机制主要是由一个混沌过程控制的,该混沌过程与激流和双重涡旋之间的非线性相互作用有关。

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