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南海北部深海潮汐的季节性变化特征
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  • 英文篇名:Seasonal variability of tides in the deep northern South China Sea
  • 作者:赵玖强 ; 张艳伟 ; 刘志飞 ; 赵玉龙 ; 王萌
  • 英文作者:Zhao J;Zhang Y;Liu Z;Zhao Y;Wang M;
  • 关键词:深海潮汐 ; 季节性变化 ; 亚惯性流 ; 中尺度涡 ; 南海北部
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:同济大学海洋地质国家重点实验室;
  • 出版日期:2019-01-29 13:42
  • 出版单位:中国科学:地球科学
  • 年:2019
  • 期:v.49
  • 基金:国家自然科学基金项目(批准号:41576005,91528304,41876048)资助
  • 语种:中文;
  • 页:JDXK201904007
  • 页数:14
  • CN:04
  • ISSN:11-5842/P
  • 分类号:111-124
摘要
深海潮汐是深海混合过程的主要能量来源,对深海环流变异和沉积物搬运具有重要的调控作用.文章利用深水锚系观测系统在南海北部2100m水深处开展了近两年的高分辨率海流剖面观测,用于研究深海潮汐的季节性变化特征.通过谱分析显示,南海北部深海潮汐以全日潮为主,且在观测区域的深海中,全日潮和半日潮以垂向第一模态结构为主.斜压全日潮具有显著的季节性变化特征,夏季最强,深度平均的最大动能达86.7cm2s-2,分别是冬季的1.5倍、春秋季的2倍;而斜压半日潮没有明显的季节性变化.通过对比发现斜压全日潮的季节性变化受控于吕宋海峡附近的正压潮.另外,观测期间有三个强中尺度涡经过锚系站位,其中一个气旋式中尺度涡对深海海流影响较小,而另外两个反气旋式中尺度涡经过研究海域时可影响全水深海流,激发强亚惯性流,对深海潮汐产生边缘强化效应,并使深海斜压全日潮冬季的异相成分增强,占全日潮的85%.同时,中尺度涡对深海海水混合的增强弱化了海水层结,导致冬季的斜压全日潮流速减弱,低于夏季.南海北部深海潮汐季节性变化为研究深海盆沉积物在不同时间尺度上的分布及搬运过程提供了重要的动力机制.
        
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