Ocean General Circulation Models Based on Hamiltonian Methods

这项工作是为了继续发展基于使用哈密顿方法导出的近似动力学方程的海洋环流数值模式。这些方程在物理上是一致的，但在数学上比现在常用的模型方程更简单。将这些方程应用于依赖于密度平流和非线性的海洋过程。

This effort is to continue the development of numerical ocean general circulation models based on approximate dynamical equations that are derived using Hamiltonian methods. The equations are physically consistent but mathematically simpler than model equations now in common use. Application of the equations will be made to ocean processes that depend on density advection and non-linearity.