With two - dimensional quasi - geostrophic motion , a series of numerical experiments are made to prove the theoretical results ； gj ）传统识别模式误差和奶始误差的方法，是把一系列的初始场输入到。
2.
The regimes of turbulence include homogeneous flows in two and three dimensions , geostrophic motions , shear flows , convection , boundary layers , stably stratified flows , and internal waves 扰流的形式包括二维和三维的均匀流动、因地球自转而引起的运动、切向流动、对流、边界层流、稳定层流和内部波动。
