walker circulation meaning in Chinese
沃克环流
沃克流
Examples
- Equatorial zonal circulation ; walker circulation
赤道纬向环流walker环流 - These phenomena are relevant to the anomaly low sst in tropic eastern pacific ( la nina ) and the strengthen of walker circulation
这些现象又与东太平洋海温的明显偏低( lani ( ? ) a )和沃克环流的加强密切相关。 - The eastward shift in the walker circulation and western wind anomolis are the possible reasons of the change of relationships between summer cross equator flows and enso
赤道太平洋西风异常及walker环流上升支的东移使得夏季越赤道气流与enso的关系产生了明显的年代际变化。 - On the surface of msta , there exists true dipole mode in the indian ocean , that ' s to say that if the temperature anomaly in the western indian ocean is positive , it is much likely that there is negative anomaly in the eastern indian ocean . dipole mode also exists in the pacific as that in the indian ocean . by virtue of the walker circulation and the similar circulation above the indian ocean , it is showed that the air - sea interaction events in the tropical pacific and the indian ocean develop with each other at the same time
由于在次表层海温距平极值面上，热带西、东印度洋的海温距平呈真正意义的偶极子模态，即当西印度洋海温距平为正(负)时，东印度洋海温距平为负(正) ，偶极子模态的海温距平分布在热带太平洋同样存在，两大洋海温距平的偶极子模态间有密切的联系，结合walker环流和印度洋上空的类似walker环流，进而指出热带印度洋和太平洋海气相互作用事件是协调发展的。 - During the years of strong monsoon , the convective activities happening in tropical india ocean and tropical west pacific and walker circulation are much stronger than that during the years of weak index , but the convective activities happening in tropical east pacific are weaker than those during the years of weak monsoon
春季热带对流活动对山东夏季降水异常的贡献比夏季更显著。强季风年与山东夏涝年相联系，热带印度洋一菲律宾群岛、南海一热带西太平洋对流活动偏强，热带东太平洋地区对流活动偏弱， walker环流加强。