| 赤道大洋驻波异常及其年际变化的理论分析 |
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| 引用本文： | 卢姁,赵艳玲,张东凌,张铭,刘赛赛.赤道大洋驻波异常及其年际变化的理论分析[J].海洋学报,2022,44(3):15-24. |
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| 作者姓名： | 卢姁 赵艳玲 张东凌 张铭 刘赛赛 |
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| 作者单位： | 1.中国人民解放军32021部队，北京 100094 |
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| 基金项目： | 国家重点研发计划高性能计算项目（2016YFB0200800）； |
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| 摘 要： | 本文采用赤道β平面近似下的线性化正压扰动方程组，引入约化重力加速度后，得到了赤道驻波异常的解析解，给出了此解的计算结果，并与实际热带太平洋和印度洋流场异常复EOF分析的模态做了比较，得到以下主要结论:赤道驻波异常的模态1，其流场异常在整个大洋为半波，呈一致的纬向流；流场异常在热带大洋中部最大，并向赤道南北两侧迅速衰减，其被限制在赤道两侧约2o的范围内。赤道驻波的模态2，其流场异常在整个大洋为1波，在大洋东、西部纬向流的流动方向相反，流场异常向赤道南北两侧衰减的程度同模态1。赤道驻波异常分别满足南北走向的东、西海岸边条件。决定赤道驻波异常在赤道两侧衰减程度的系数，其仅与约化重力加速度和上层海水标准深度之乘积的平方根值成反比；当该值取得相同时该衰减程度也相同。赤道驻波异常的振荡频率与模态序号及上述平方根值成正比，与热带大洋宽度成反比；模态序号越低，该宽度越大，则该频率越低，相应振荡周期也越长；模态1的振荡周期最长。当取各参数为典型值，并取模态序号为1，再分别取热带太平洋和印度洋的宽度时，对赤道驻波异常计算的结果表明，其与实际相应海洋上层流场异常复EOF分析中得到的第一模态空间分布和年际变化相一致；这意味着此复EOF分析第一模态的本质是赤道驻波异常，这也表明该驻波异常在实际大洋中确实存在，并推断该驻波异常是ENSO和印度洋偶极子的形成机制之一。
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| 关 键 词： | 赤道驻波 太平洋 印度洋 年际变化 |
| 收稿时间： | 2021-01-28 |
Theoretical analysis of anomalous equatorial ocean stationary wave and its interannual variability |
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| Lu Xu,Zhao Yanling,Zhang Dongling,Zhang Ming,Liu Saisai.Theoretical analysis of anomalous equatorial ocean stationary wave and its interannual variability[J].Acta Oceanologica Sinica (in Chinese),2022,44(3):15-24. |
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| Authors: | Lu Xu Zhao Yanling Zhang Dongling Zhang Ming Liu Saisai |
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| Affiliation: | 1.Unit 32021, PLA, Beijing 100094, China2.Unit 31010, PLA, Beijing 100081, China3.Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China4.Laboratory of Atmospheric Circulation and Short-range Climate Forecast, Meteorological and Oceanographic College, National University of Defense Technology, Nanjing 211101, China |
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| Abstract: | In this paper, using the equatorial beta-plane approximation of the linear barotropic perturbation equations and introducing the reduced gravitational acceleration, we obtain the analytical solutions of anomalous equatorial ocean stationary wave and give the calculation results of the solutions. Then we compare the results with the modes of complex EOF analysis about abnormal circulation of the real tropical Pacific Ocean and Indian Ocean. The main conclusions are: in the first mode of anomalous equatorial ocean stationary wave, the current disturbance throughout the whole ocean is the half wave, which appears as the consistent zonal flow. The maximum disturbance appears at the middle of the tropical ocean and decays rapidly from equator to north and south, which is restricted in about 2 degree range on both sides of the equator. In the second mode, the current disturbance throughout the whole ocean is the full wave and has the opposite flow direction at east and west of the ocean. The degree of the attenuation of the current disturbance from equator to north and south is as that of the first mode. Anomalous equatorial ocean stationary wave meets the boundary conditions of the east and west coast directing along the longitude. The coefficient is inversely proportional to the square root of the product of the reduced gravity acceleration and the upper water standard depth, which determines the decay rate of anomalous equatorial ocean stationary wave on both sides of the equator. If the square root values take the same, the decay rates are the same. The oscillation frequency of anomalous stationary wave is proportional to the modal number and the square root values, which is inversely proportional to the width of tropical ocean. The modal number is lower and the width is larger, the frequency is lower and the corresponding oscillation period is longer; the first mode of the oscillation period is the longest. Taking every parameters as the typical values and the modal number as one, then taking the width of the equatorial Pacific Ocean and Indian Ocean respectively, the calculation results show that the spatial distribution and interannual variability of the first mode are the same as the corresponding mode of the real abnormal circulation obtaining from the complex EOF analysis; this means that the nature of the first mode above is the anomalous equatorial ocean stationary wave and the anomalous stationary wave is one of the generating mechanism of ENSO and IOD. |
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