风生环流

赤道大洋定常风生环流的理论模型

A Theoretical Model for the Steady Equatorial Ocean Wind-driven Circulation

准地转大洋风生环流的格子Boltzmann数值模拟

Lattice Boltzmann modeling for quasi-geostrophic model of wind-driven ocean circulation

风生环流机制模式的格子Boltzmann数值模拟热带西太平洋环流动力结构分析与模拟

Lattice Boltzmann Modeling for Mechanistic Models of Wind-driven Ocean Circulation Dynamic Structure of Ocean Circulation in the Tropical Western Pacific Ocean and Its Simulation

北部湾风生环流的数值研究

A numerical study on wind - driven circulation in the Beibu Gulf

最后对风生环流和正压环流的特征进行了分析和讨论。

Finally , we discuss and analyse the structure of the wind-dviven circulation and the barotropic circulation .

麻醉维持期循环稳定。3~4h后东湖水体形成流速在厘米量级的稳定的风生环流。

The circulation was stable during anesthesia maintenance . The stable circulation flow velocity is centimeter magnitude order .

海洋密度分布不均一产生的热盐环流，海面风应力驱动的风生环流，天体引潮力所产生的潮致余流等等，是海洋环境发生变化的基本动力或原因。

The basic power or reason , such as thermohaline circulation , wind-driven current or tidal residual circulation , can make ocean environment changing .

风生环流在近岸区显著，在冬季和夏季分别形成沿岸南下和北上的风生流，具有冬强夏弱的特点；

Wind-driven circulations are more evident near coast , in winter strong wind-driven circulations flow south along the coast while in summer flow north weakly .

在南海南部主要是风生环流，源自粤西沿岸的水体在东北季风的作用下顺南海西边界岸线向南流动，形成一支相当强的西边界流；

It is mainly wind driven current in the southern SCS , the water from alongshore of western Guangdong is driven by the northeast monsoon and then flows southward along the western boundary shorelines of the SCS , thus a rather strong western boundary current is formed ;

南海风生正压环流动力机制的数值研究

On mechanisms numerical study on the dynamics of wind driven barotropic circulation in the South China Sea

渤海夏季潮致-风生-热盐环流的数值诊断计算

Numerical diagnostic simulation of summertime tide-induced , wind-driven and thermohaline currents in the Bohai Sea