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南海西北部上层海洋对连续台风的近惯性响应
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  • 英文篇名:Upper ocean near-inertial response to the passage of two sequential typhoons in the northwestern South China Sea
  • 作者:马永贵 ; 张书文 ; 齐义泉 ; 经志友
  • 英文作者:Ma Y;Zhang S;Qi Y;Jing Z;
  • 关键词:连续台风 ; 近惯性振荡 ; 近惯性能量传播
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:广东海洋大学海洋与气象学院;青岛海洋科学与技术国家实验室区域海洋动力学与数值模拟功能实验室;河海大学海洋学院;中国科学院南海海洋研究所热带海洋环境国家重点实验室;
  • 出版日期:2019-01-30 10:12
  • 出版单位:中国科学:地球科学
  • 年:2019
  • 期:v.49
  • 基金:国家重点研发计划重点专项项目(编号:2016YFC14001403);; 国家自然科学基金面上项目(批准号:41676008,40876005);; 全球变化与海气相互作用专项国际合作项目(编号:GASI-IPOVI-04)资助
  • 语种:中文;
  • 页:JDXK201904008
  • 页数:10
  • CN:04
  • ISSN:11-5842/P
  • 分类号:125-134
摘要
文章基于2011年9~11月南海西沙潜标观测资料,研究了西沙海域上层海洋对连续台风Nesat(1117)和Nalgae(1119)过境的近惯性响应.结果表明:两个台风过境都产生了强烈的近惯性振荡,且台风路径右侧的近惯性流速明显大于左侧. Nesat引起的近惯性内波平均垂向相速度为0.25cm s~(-1),垂向群速度为0.85m h-1,垂向波长为350m.Nalgae所引起的近惯性内波垂向相速度和群速度均小于Nesat,垂向波长仅为Nesat的1/2.两个台风引起的近惯性能量下传深度存在明显差异, Nalgae约为200m,而Nesat可下传至300m.产生这一差异的主要原因是Nesat引起的近惯性能量不易耗散,同时能够以较快的速度向深海传播.此外,两个台风引起的近惯性内波频率都存在明显的蓝移现象. Nesat引起的近惯性内波频率在100~150m深度受多普勒频移的影响明显增大;然而Nalgae引起的近惯性内波频率却在100~150m深度显著减小,这是由于两个台风过境期间,西沙海域背景场涡度差异所致.
        
引文
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