{"title":"The modeling system of the Ocean Current","authors":"Dongfang Yang, Xiaoju Zhang, S. Manickam","doi":"10.1145/3548608.3559291","DOIUrl":null,"url":null,"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.","PeriodicalId":201434,"journal":{"name":"Proceedings of the 2022 2nd International Conference on Control and Intelligent Robotics","volume":"167 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-06-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of the 2022 2nd International Conference on Control and Intelligent Robotics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1145/3548608.3559291","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
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.