论文部分内容阅读
迄今为止,我们在如下领或中尚存在认识上的差距:1.海洋表层温度大尺度变化的物理学实质,这些变化与大洋环流和大气过程变化特点的关系,对于大气和海一气间大尺度相互作用的反馈;2.海洋1500-2000米表层水团水平环流与大洋深层水环流之间的联系;3.海洋深处垂直环流的细微结构;4.所有天然尺度(从几百公里到几百米)的海洋涡旋在起源及其动力学方面的差别;5.多种天气尺度涡量的特别《长生》的物理学原因:6.确定天气尺度涡量缓和的独特过程;7.确定海洋长期存在的急剧变化的温跃锋面的准稳定锋面的动力学。8.海洋锋面的三维结构;9.决定海洋锋面出现不稳定性时的诸动力要素;10.组成
So far, we still have the following gaps in cognition: 1. The physical essence of the large-scale changes in the surface temperature of the ocean and the relationship between these changes and the characteristics of ocean circulation and atmospheric processes. For large-scale Interaction; 2. The relationship between the 1500-2000 m surface water level circulation in the ocean and the deep oceanic water circulation; 3. the fine structure of the vertical circulation in the depths of the ocean; 4. all the natural scales (from several hundred kilometers to several A hundred meters) of marine vortex in the origin and dynamics of the difference; 5. A variety of weather-scale vorticity special “longevity” of the physical reasons: 6. Determine the weather scale vorticity mitigation unique process; Oceanic long-term, rapidly changing, thermoeletropic quasi-stable frontier dynamics. 8. The three-dimensional structure of the ocean front; 9. The dynamical elements that determine the instability of the front of the ocean; 10. The composition