Baroclinic structure of oceanic rings
The baroclinic structure of oceanic rings is studied through observational data and numerical simulation. Based on the newly discovered geostrophic empirical mode (GEM), which represents a low-dimensional coherent structure in oceanic baroclinic fields, we are able to construct equivalent-barotropic ring solutions that describe the observed velocity and density distribution. Unlike the previous layer-model approach, the GEM vortex solution is intended for continuously stratified fluids. It allows us to conduct a series of numerical experiments with general circulation models, from which the phenomenon that geophysical vortex tends to evolve to a vertical alignment state with horizontally axisymmetric shape is investigated.
oceanic rings baroclinic geostrophic empirical mode vertical alignment axisymmetrization
L.Zhang C.Sun
Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071 China;Graduate School of Chine Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071 China
国际会议
The Fifth International Conference on Fluid Mechanics(第五届国际流体力学会议)
上海
英文
2007-08-15(万方平台首次上网日期,不代表论文的发表时间)