The modeling system of the Ocean Current

Dongfang Yang, Xiaoju Zhang, S. Manickam
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Abstract

According to the migration theory of Yang Dongfang material content proposed by the author and taking material content as indicator, this article determined the transportation process of material content by ocean current, and obtained the moving trajectory of ocean current, where the ocean current was defined as Yang Dongfang Ocean Current. Taking Pb content as indicator, this article presented the migration process of Pb content in the waters of Jiaozhou Bay under the transportation of ocean current and the moving trajectory of ocean current. Based on the migration theory of Yang Dongfang material content, the results indicated that the ocean current in open sea brought high Pb content to Jiaozhou Bay and left the moving trajectory inside Jiaozhou Bay as the Pb content decreased. The author established a block diagram to elaborate it. Moreover, the results further revealed that the unit water body followed the ocean current from the mouth of the bay along the nearshore waters in the bay and then returned to the mouth of the bay in a counterclockwise direction. Then, under the combined action of ocean current and tides, the unit water body showed a zigzag-shaped movement from east to north and then to the west along the nearshore waters. The center of this bay was almost unaffected by the unit water body. The unit water body took the center of the bay as the center of the circle, and moved in a zigzag shape along the edge. Therefore, the author proposed the movement mechanism of Yang Dongfang Ocean Current, revealed the moving of Yang Dongfang Ocean Current and depicted the submarine geomorphy, such as Jiaozhou Bay. Applying the movement mechanism of Yang Dongfang Ocean Current, this article presented the moving trajectory, direction and position of Yang Dongfang Ocean Current. Similarly, in the southern hemisphere, the pathway and position of the Yang Dongfang Ocean Current remained the same while the direction of the current was opposite. A block diagram was also built to elaborate it.
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洋流的模拟系统
本文根据作者提出的杨东方物质含量迁移理论,以物质含量为指标,确定了物质含量受洋流的搬运过程,得到了洋流的移动轨迹,其中将洋流定义为杨东方洋流。以Pb含量为指标,研究了胶州湾海域Pb含量在洋流输送作用下的迁移过程和洋流的移动轨迹。基于杨东方物质含量迁移理论,表明远海洋流将高Pb含量带入胶州湾,并随着Pb含量的降低在胶州湾内部留下移动轨迹。作者建立了一个框图来阐述它。此外,结果进一步揭示了单位水体从海湾口沿海湾近岸水域跟随洋流,然后沿逆时针方向返回海湾口。然后,在洋流和潮汐的共同作用下,单元水体沿近岸水域呈现由东向北再向西的“之”字形运动。这个海湾的中心几乎不受单位水体的影响。单元水体以海湾中心为圆心,沿边缘呈之字形移动。在此基础上,提出了杨东方洋流的运动机制,揭示了杨东方洋流的运动规律,描绘了胶州湾等海底地貌。利用杨东方洋流的运动机理,给出了杨东方洋流的运动轨迹、方向和位置。同样,在南半球,杨东方洋流的路径和位置保持不变,但方向相反。还制作了一个框图来详细说明。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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