| WANG Yu,LAN Jian,CUI Fengjuan. 2014. Effect of nonlinear advection on the Indian Ocean diploe asymmetry. Acta Oceanologica Sinica, 33(1):77－82 |
| Effect of nonlinear advection on the Indian Ocean diploe asymmetry |
| Effect of nonlinear advection on the Indian Ocean diploe asymmetry |
| Received:August 05, 2012 Revised:December 17, 2013 |
| DOI：10.1007/s13131-014-0420-y |
| Key words:asymmetry of Indian Ocean dipole dynamical effect heat budget nonlinear advection |
| 中文关键词: asymmetry of Indian Ocean dipole dynamical effect heat budget nonlinear advection |
| 基金项目:The National Natural Science Foundation of China under contract Nos 41276011, 41221063 and 41130859; the National Basic Research Program of China under contract No. 2012CB417404. |
| Author Name | Affiliation | E-mail | | WANG Yu | Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266100, China
Department of Oceanography, Ocean University of China, Qingdao 266100, China | | | LAN Jian | Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266100, China
Department of Oceanography, Ocean University of China, Qingdao 266100, China | lanjian@ouc.edu.cn | | CUI Fengjuan | Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266100, China
Department of Oceanography, Ocean University of China, Qingdao 266100, China | |
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| Abstract: |
| The asymmetry of sea surface temperature anomaly (SSTA) amplitudes between the positive and negative phases of the Indian Ocean dipole (IOD) are studied. The dynamic effects on it are analyzed using a hybrid coordinate ocean model (HYCOM). It suggests that the IOD is still asymmetric even when forced by a symmetric wind stress, and the asymmetry of the SSTA in the eastern pole is strong while that in the western pole is almost insignificant during the mature phase (September-November (SON)). Thus, the IOD asymmetry is primarily caused by the asymmetry in the IODE. A heat budget analysis is also conducted for the mixedlayer temperature in the eastern Indian Ocean (IODE), which indicates that a nonlinear ocean advection cools both the positive and negative IOD events. Therefore, the nonlinear ocean advection is responsible for the asymmetry of the IOD. |
| 中文摘要: |
| The asymmetry of sea surface temperature anomaly (SSTA) amplitudes between the positive and negative phases of the Indian Ocean dipole (IOD) are studied. The dynamic effects on it are analyzed using a hybrid coordinate ocean model (HYCOM). It suggests that the IOD is still asymmetric even when forced by a symmetric wind stress, and the asymmetry of the SSTA in the eastern pole is strong while that in the western pole is almost insignificant during the mature phase (September-November (SON)). Thus, the IOD asymmetry is primarily caused by the asymmetry in the IODE. A heat budget analysis is also conducted for the mixedlayer temperature in the eastern Indian Ocean (IODE), which indicates that a nonlinear ocean advection cools both the positive and negative IOD events. Therefore, the nonlinear ocean advection is responsible for the asymmetry of the IOD. |
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