| FAN Haimei,LI Bingrui,XU Ren,ZHANG Zhenglong,LI Yihong.Adjustment time of the first baroclinic Rossby wave in the global oceans[J].Acta Oceanologica Sinica,2006,(6):15-21 |
| Adjustment time of the first baroclinic Rossby wave in the global oceans |
| Adjustment time of the first baroclinic Rossby wave in the global oceans |
| 投稿时间：2005-11-11 修订日期：2006-06-17 |
| DOI： |
| 中文关键词: first baroclinic Rossby wave global Rossby adjustment adjustment time |
| 英文关键词:first baroclinic Rossby wave global Rossby adjustment adjustment time |
| 基金项目: |
| 作者 | 单位 | E-mail | | FAN Haimei | East China Sea Environment Monitoring Center, State Oceanic Administration, Shanghai 200137, China | ffhhmmdawn@yahoo.com.cn | | LI Bingrui | Physical Oceanography Laboratory, Polar Research Institute of China, Shanghai 200136, China | | | XU Ren | East China Sea Environment Monitoring Center, State Oceanic Administration, Shanghai 200137, China | | | ZHANG Zhenglong | East China Sea Environment Monitoring Center, State Oceanic Administration, Shanghai 200137, China | | | LI Yihong | East China Sea Environment Monitoring Center, State Oceanic Administration, Shanghai 200137, China | |
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| 中文摘要: |
| According to the freely linear Rossby wave theory, global 1°×1° climatology of Rossby deformation radius and phase speed are studied under the flat bottom fluid approximation.Geographical variations in the contours of the phase speed are very similar to those of the Rossby radius of formation, which are mainly affected by stratification, rotation, water depth, topography, etc.The basin-crossing time of the first baroclinic Rossby wave is obtained and analyzed in the global ocean basins.The results are useful to learn the importance of Rossby wave and the adiabatic adjustment of large-scale ocean circulation. |
| 英文摘要: |
| According to the freely linear Rossby wave theory, global 1°×1° climatology of Rossby deformation radius and phase speed are studied under the flat bottom fluid approximation.Geographical variations in the contours of the phase speed are very similar to those of the Rossby radius of formation, which are mainly affected by stratification, rotation, water depth, topography, etc.The basin-crossing time of the first baroclinic Rossby wave is obtained and analyzed in the global ocean basins.The results are useful to learn the importance of Rossby wave and the adiabatic adjustment of large-scale ocean circulation. |
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