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Effect of nonlinear advection on the Indian Ocean diploe asymmetry
作者姓名:WANG Yu  LAN Jian  CUI Fengjuan
作者单位:Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266100, China;Department of Oceanography, Ocean University of China, Qingdao 266100, China;Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266100, China;Department of Oceanography, Ocean University of China, Qingdao 266100, China;Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266100, China;Department of Oceanography, Ocean University of China, Qingdao 266100, China
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.
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.

关 键 词:印度洋偶极子  不对称性  非线性  平流  海表温度距平  海洋模式  IOD  风应力强迫
收稿时间:8/5/2012 12:00:00 AM
修稿时间:2013/12/17 0:00:00

Effect of nonlinear advection on the Indian Ocean diploe asymmetry
WANG Yu,LAN Jian,CUI Fengjuan.Effect of nonlinear advection on the Indian Ocean diploe asymmetry[J].Acta Oceanologica Sinica,2014,33(1):77-82.
Authors:WANG Yu  LAN Jian and CUI Fengjuan
Institution:Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao 266100, China;Department of Oceanography, Ocean University of China, Qingdao 266100, China
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.
Keywords:asymmetry of Indian Ocean dipole  dynamical effect  heat budget  nonlinear advection
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