| Wang Jia,Moto Ikeda.A three-dimensional ocean general circulation model for mesoscale eddies——Ⅱ Diagnostic analysis[J].Acta Oceanologica Sinica,1997,(1):29-43 |
| A three-dimensional ocean general circulation model for mesoscale eddies——Ⅱ Diagnostic analysis |
| A three-dimensional ocean general circulation model for mesoscale eddies——Ⅱ Diagnostic analysis |
| 投稿时间：1996-03-15 修订日期：1996-07-28 |
| DOI： |
| 中文关键词: |
| 英文关键词: |
| 基金项目: |
|
| 摘要点击次数: 779 |
| 全文下载次数: 554 |
| 中文摘要: |
| A three-dimensional density field associated with mesoscaie unstable waves generated by the 3-D,primitive-equation model (Wang and Ikeda,1996) is provided to the quasi-geostrophic pressure tendency and ω-equations,and to the (ageostrophic) Q-vector equation.Diagnostic analyses,analogous to the approaches in meteorology:ω-equation and Q-vector method,are for the first time developed to examine the mesoscaie dynamical processes and mechanisms of the unstable waves propagating in the mid-latitude ocean.The weaknesses and strengths of these two diagnostic approaches are evaluated and compared to the model results.The Q-vector method is then recommended to diagnose the vertical motion associated with the mesoscaie dynamics from a hydrographic CTD (conductivity-temperature-depth) array,while the quasi-geostrophic equations produce some small-scale features (errors) in the diagnosed fields. |
| 英文摘要: |
| A three-dimensional density field associated with mesoscaie unstable waves generated by the 3-D,primitive-equation model (Wang and Ikeda,1996) is provided to the quasi-geostrophic pressure tendency and ω-equations,and to the (ageostrophic) Q-vector equation.Diagnostic analyses,analogous to the approaches in meteorology:ω-equation and Q-vector method,are for the first time developed to examine the mesoscaie dynamical processes and mechanisms of the unstable waves propagating in the mid-latitude ocean.The weaknesses and strengths of these two diagnostic approaches are evaluated and compared to the model results.The Q-vector method is then recommended to diagnose the vertical motion associated with the mesoscaie dynamics from a hydrographic CTD (conductivity-temperature-depth) array,while the quasi-geostrophic equations produce some small-scale features (errors) in the diagnosed fields. |
|
查看全文
查看/发表评论 下载PDF阅读器 |
| 关闭 |
|
|
|