| 1. | Key areas of air - sea interaction in global oceans and their climatic features
全球海气相互作用关键区及区内气候特征分析 |
| 2. | Interaction of air - sea in the middle latitudes and decadal climatic oscillations
海气相互作用与年代际气候振荡可能机制初探 |
| 3. | So , it is more likely the tropical processes themselves lead to enso decadal variability
可见， enso的年代际变化可能只是热带范围内的海气相互作用过程。 |
| 4. | Modes of air - sea interactions in the indian ocean and their relationships with the rainfall over china as revaled by svd analysis
揭示的印度洋海气相互作用模态及其与中国降水的联系 |
| 5. | 3 ) the upper ocean participates the process of air - sea interaction both in winter and summer in the tropical pacific but only in winter in the north pacific
3 )浅层海洋参与海气相互作用在热带太平洋区域冬、夏均存在，而在北太平洋区域仅限于冬季。 |
| 6. | Diagnostic analysis and contrast are performed in air - sea data and their interaction between the north pacific and the tropical pacific by means of harmonic analysis and svd
使用谐波分析及奇异值分解( svd )方法分析比较了北太平洋、热带太平洋区域的海气资料及海气相互作用。 |
| 7. | 2 ) the leading svd modes of interdecadal variability are indicative of stronger statistical significiance in the north pacific than in the tropical pacific , while the conclusion is contrary as for interannual variability
2 )年代际变化海气相互作用北太平洋区域较热带太平洋区域显著，年际变化海气相互作用热带太平洋区域较北太平洋区域显著。 |
| 8. | Results of recent observation and numerical experiments show that prominent difference exists between air - sea interaction in tropical and in mid - latitude , and work is not enough related to the impact of persistent ssta on the circulation considering different district in pacific
观测分析和数值模拟结果表明中纬度与热带地区的海气相互作用存在差异，但深入讨论不同关键海区的持续性ssta对大气环流影响的工作还不充分。 |
| 9. | 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。 |
| 10. | 4 ) air - sea interaction retain its character throughtout the seasonal cycle in the tropical pacific , but it is not the same in the north pacific ; and there are also relationships in the two areas : 1 ) for the interdecadal time scale , there is the same abrupt change both in the north pacific and in the tropical pacific , especially in winter
4 )热带太平洋区域海气相互作用有较好的季节一致性；而北太平洋区域海气相互作用季节差异较大。区域间主要联系为： 1 )两个区域主要的年代际跃变点出现时间接近，这在冬季反映最明显。 |
