Frontier Science Center for Deep Ocean Multispheres and Earth System
(FDOMES) and Physical Oceanography Laboratory, Ocean University of China,
Qingdao, 266100, China
Frontier Science Center for Deep Ocean Multispheres and Earth System
(FDOMES) and Physical Oceanography Laboratory, Ocean University of China,
Qingdao, 266100, China
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI), Bremerhaven, Germany
Shi Qiu
Frontier Science Center for Deep Ocean Multispheres and Earth System
(FDOMES) and Physical Oceanography Laboratory, Ocean University of China,
Qingdao, 266100, China
Jiaqi Guo
Frontier Science Center for Deep Ocean Multispheres and Earth System
(FDOMES) and Physical Oceanography Laboratory, Ocean University of China,
Qingdao, 266100, China
Frontier Science Center for Deep Ocean Multispheres and Earth System
(FDOMES) and Physical Oceanography Laboratory, Ocean University of China,
Qingdao, 266100, China
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Total article views: 3,350 (including HTML, PDF, and XML)
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The Oceanic Regional Circulation and Tide Model (ORCTM) is developed to reproduce internal solitary wave dynamics. The three-dimensional nonlinear momentum equations are involved with the nonhydrostatic pressure obtained via solving the Poisson equation. The validation experimental results agree with the internal wave theories and observations, demonstrating that the ORCTM can successfully describe the life cycle of nonlinear internal solitary waves under different oceanic environments.
The Oceanic Regional Circulation and Tide Model (ORCTM) is developed to reproduce internal...
