首页|基于潜标观测的黑潮-亲潮混合区近惯性能量季节变化特征研究

基于潜标观测的黑潮-亲潮混合区近惯性能量季节变化特征研究

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近惯性内波广泛存在于全球海洋,是维持深层海洋跨等密度面湍流混合及海洋层结的重要能量来源.基于黑潮-亲潮混合区的多年深海潜标数据,分析了:(1)该海域近惯性内波及其能量的季节变化特征与影响因素,(2)上层和深层近惯性运动的频率、波数谱及垂向分布等特征.结果表明,该海域存在丰富的近惯性动能,无论海洋上层还是深层均呈现显著的冬季强、夏季弱的季节变化特征,冬季(12~2月)上层的近惯性能量可占全年能量的41%,深层近惯性信号同样显著,同潮汐信号相当.平板模型分析表明,该区域近惯性动能的季节循环特征主要受风场的季节变化所主导,同时受到黑潮延伸体流轴的摆动调制.
CHARACTERIZATION OF SEASONAL VARIATION OF NEAR-INERTIAL ENERGY IN KUROSHIO-OYASHIO MIXED ZONE BASED ON MOORING OBSERVATIONS
Near-inertial waves(NIWs)are widespread in the global ocean,and are a significant energy source for turbulent diapycnal mixing in the deep ocean to maintain ocean stratification.Based on multi-year deep-sea mooring data collected in the Kuroshio-Oyashio mixed zone,we focused on the seasonal variations and the dominant factors in determining near-inertial kinematic energy in this region,and the characteristics of wave frequency,wavenumber spectrum,and vertical distribution of near-inertial motions in the upper and deep ocean.Results revealed the presence of abundant near-inertial kinetic energy in this region.Both the upper and deep ocean layers exhibit notable seasonal variation,and are characterized by pronounced intensification in winter and weakening in summer.Specifically,in winter months,near-inertial energy in the upper layer can contribute to 41%of the total annual energy.Moreover,the near-inertial energy in the deep-layer ocean is equally significant,being comparable to the tidal signals.The slab model suggests that these seasonal cycles of near-inertial energy are primarily driven by external wind forcing,with additional influence from the northward shift of the Kuroshio extension axis.

Kuroshio-Oyashio mixed zonenear-inertial waveseasonal variationmooring observation

范中祥、孙冰溶、陈朝晖

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中国海洋大学深海圈层与地球系统前沿科学中心/物理海洋教育部重点实验室 山东青岛 266100

中国海洋大学未来海洋学院 山东青岛 266100

黑潮-亲潮混合区 近惯性内波 季节变化 潜标观测

国家自然科学基金青年科学基金项目国家自然科学基金面上基金项目中央高校基本科研业务费专项青岛市博士后基金

42106015号42176218号202072009号862105040025号

2024

海洋与湖沼
中国海洋湖沼学会 中国科学院海洋研究所

海洋与湖沼

CSTPCD北大核心
影响因子:0.737
ISSN:0029-814X
年,卷(期):2024.55(2)
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