Three-Dimensional Structure of the Subtropical Gyres

最近的海洋动力学模型试图将表层或侧面边界附近的过程耦合起来。很难将两者的物理学整合到分析模型中。这项研究试图使用海洋温跃层的分析模式来考虑近地表和西部边界层过程。要使用的模型将在垂直方向上分层或连续分层。

Recent models of ocean dynamics have attempted to couple the processes at the surface or near the side boundaries. It has been difficult to integrate the physics of both into analytical models. This investigation seeks to use anlaytical models of the ocean thermocline to consider the near surface and western boundary layer processes. The models to be used will be either layered or continuously stratified in the vertical direction.