1·The multiple equilibria and their catastrophe of the low-order barotropic model are studied.
本文研究了低阶正压模式的多平衡态和平衡态的突变。
2·In this paper, a simple barotropic model is used to study the interactions of tropical forcing responses and wintertime basic flow.
本文使用简单的正压模式，研究了热带强迫响应和冬季基本气流的相互作用。
3·The split explicit integration scheme for the barotropic primitive equation model is investigated for the stability and accuracy.
本文用正压原始方程模式考察了分离显式积分方案的稳定性和精确性。
4·Numerical simulation of currents of the western North Tropical Pacific Ocean have been carried out by using a barotropic primitive equation model with finer horizontal resolution.
用一个水平分辨率比较高的非线性正压模式，对热带西太平洋海域里的海流进行了数值模拟。
5·A barotropic numerical model is employed to explain some of the observed features. Reasonable simulation of the circulation in the northeast part of SCS has been found.
使用一个正压数值模式，解释了一些观测到的特征，得到了南海东北部环流合理的模拟。
6·A simple LB model is present to numerically solve the quasi-geostrophic barotropic equivalent vorticity equation at first.
首先，本文建立了一个求解准地转相当正压涡度方程的LB模型。
7·The stability and the solutions of linear and nonlinear topographically generated Rossby Waves were discussed by using a barotropic semi-geostrophic model.
本文在半地转概念下，讨论了线性和非线性地形罗斯贝波的稳定性及其解。
8·In this paper barotropic circulations in the Huanghai Sea and East China Sea are simulated numerically with a dynamic model proposed in a previous paper.
依据黄、东海环流的的动力学模型，运用“流速分解法”对黄、东海正压环流进行了数值模拟。
9·A divisional barotropic and baroclinic connection model is employed, emphasizing on studying the response of the South China Sea (SCS) circulation to the transition of monsoon in different ways.
通过利用一个分区性的正压、斜压衔接模式，重点考察了南海环流对于以不同方式变化的季风转变时的响应。