首页|阿古拉斯流域亚中尺度过程的能量分析

阿古拉斯流域亚中尺度过程的能量分析

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本文基于(1/48)°MITgcm数值模拟结果,通过频率-波数谱分析等方法分离地转平衡和非地转运动,分析了阿古拉斯流域亚中尺度的分布特征,讨论了其季节性变化的主要影响因素.结果表明,阿古拉斯流域亚中尺度过程具有冬强夏弱的显著季节变化特征,混合层斜压不稳定是影响该流域亚中尺度季节性差异的主要原因.此外,在涡动能较强的区域,地转平衡运动始终主导亚中尺度过程,季节性变化较小;在涡动能较弱的区域,地转平衡与非地转分量具有明显的季节性差异,局地混合层浅化可能是导致夏季非地转分量贡献增加的主要机制.本文研究结果有助于进一步探究阿古拉斯流域亚中尺度的季节性变化及其主导因素,地转平衡与非地转运动的有效分离加强了我们对海洋多尺度之间能量传递的理解.
Energy analysis of submesoscale processes in the Agulhas current system
Based on the high-resolution oceanic numerical model product of MITgcm with a resolution of(1/48)°,the geostrophic balanced motion and unbalanced wave motion are decomposed via the frequency-wavenumber spec-trum analysis method to analyze the distribution of submesoscale characteristics and diagnose the main factors af-fecting their seasonal variations in the Agulhas current system.The results show that the submesoscale processes in the Agulhas current system have a significant seasonal distribution with strong features in winter but weak features in summer.The mixed layer baroclinic instability is the main reason affecting the submesoscale seasonal differ-ences in the area.In addition,the geostrophic balanced motions are predominant in the submesoscale process in the regions with stronger eddy kinetic energy(EKE)and have no obvious seasonality.For the regions with weaker EKE,the balanced and unbalanced geostrophic motions show significant seasonality,where the local mixing layer shallowness is responsible for the increase of the unbalanced kinetic energy in summer.Our analysis helps to fur-ther clarify the characteristics of submesoscale seasonal variation and its primary factors in the Agulhas current sys-tem.The effective separation of geostrophic balanced and unbalanced motion enhances our understanding of en-ergy transformation between multiscale processes in the ocean.

Agulhas current systemsubmesoscale processgeostrophic balanced motionunbalanced wave motiontrans-ition scale

赵若楠、李刚、何宜军

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南京信息工程大学 海洋科学学院,江苏 南京 210044

自然资源部空间海洋遥感与应用重点实验室,北京 100081

崂山实验室 区域海洋动力学与数值模拟功能实验室,山东 青岛 266237

阿古拉斯流域 亚中尺度过程 地转平衡运动 非地转运动 过渡尺度

国家自然科学基金重大仪器设备研制项目

42027805

2024

海洋学报(中文版)
中国海洋学会

海洋学报(中文版)

CSTPCD北大核心
影响因子:1.044
ISSN:0253-4193
年,卷(期):2024.46(1)
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