The timescales Analysis of long-term variability of oceanic circulation forced by the stationary wind in a two-layer ocean. PART 2. Spectral analysis
Using numerical simulation of two-layer ocean with the layer depths corresponding to real oceanic conditions under the outer stationary vorticity flux and constant dissipation factors the investigation of the development of a large-scale circulation has been provided. There have been discovered the dependence of large-scale total energy circulation oscillations on the position of the enstrophy spectra mass-center.