The wind field is residualcirculation calculated from diabatic rate.
模式中应用的流场来自根据加热率计算得到的剩余环流。
2
The horizontal and vertical structures of tidal currents were obtained and the inter-tidal Eurlarian residualcirculation was analyzed.
模拟获得了三维潮流水平与垂直分布结构以及若干个潮致余流涡的水平分布状况。
3
ENSO lead to a change in the aerosol delivery by affecting the residualcirculation, and in turn lead to these differences of the aerosol distribution mentioned above.