海洋学研究 ›› 2019, Vol. 37 ›› Issue (1): 75-82.DOI: 10.3969/j.issn.1001-909X.2019.01.010

• 研究论文 • 上一篇    下一篇

天津港主航道连续观测点潮流和余流特征分析

张安民1,2, 宁一伟1, 王晨旭1, 张豪1, 刘荣霞1, 孙朝辉3   

  1. 1.天津大学 海洋科学与技术学院,天津 300072;
    2.天津市港口环境监测工程技术中心,天津 300072;
    3.自然资源部 第二海洋研究所,浙江 杭州 310012
  • 收稿日期:2018-11-03 修回日期:2018-11-29 出版日期:2019-03-15 发布日期:2022-11-21
  • 作者简介:张安民(1966-),男,安徽亳州市人,博士,研究员,主要从事海洋测绘、e航海等研究。E-mail:anmin_zhang@126.com
  • 基金资助:
    国家重点研发计划基金项目资助(2018YFC1407400);天津市科技支撑计划基金项目资助(2015F3-0004)

Study on the characteristics of tidal and residual currents on continuous observation near the main channel of Tianjin Port

ZHANG An-min1,2, NING Yi-wei1, WANG Chen-xu1, ZHANG Hao1, LIU Rong-xia1, SUN Chao-hui3   

  1. 1. School of Marine Science and Technology, Tianjin University, Tianjin 300072, China;
    2. Tianjin Port Environmental Monitoring Engineering Center, Tianjin 300072, China;
    3. Second Institute of Oceanography, MNR, Hangzhou 310012, China
  • Received:2018-11-03 Revised:2018-11-29 Online:2019-03-15 Published:2022-11-21

摘要: 基于天津港主航道连续观测点31 d的实测海流资料,利用调和分析对主航道潮流和余流特征进行研究,同时结合同步风速资料研究风对表层余流的影响。结果表明:(1)航道附近属于弱流海区,表层平均流速为31.4 cm/s,流速总体上由表至底逐渐减小,流速方向大致集中在NW—SE向。(2)观测海域潮流以正规半日往复潮占主导,优势分潮为M2,浅水分潮较为显著,涨潮流流速大于落潮流流速。(3)观测期间表层平均余流流速为2.8~13.8 cm/s,随着深度增加余流流速逐渐减小,方向大多为NW向。该站表层余流受风的影响显著,东南风将使余流方向偏向西北。

关键词: 天津港, 调和分析, 潮流, 余流

Abstract: The characteristics of the tidal and residual currents were investigated via the harmonic analysis based on the 31-day duration current observations at S station near the main channel of Tianjin Port. Effects of the local wind on the surface residual currents were explored in combination with the simultaneous wind velocities data. It is found that: (1)Tianjin Port belongs to the weak-current sea area, and the average velocity of the surface currents is about 31.4 cm/s. The current velocity generally decreases from the top to the bottom, and the main current direction is along the northwest-southeast. (2)The sea area is dominated by the regular semidiurnal tidal currents with a significant to-and-fro movement. The dominant tide component is M2, and the shallow water tide is also remarkable over there. The flood currents velocities are larger than the ebb currents. (3)The average residual currents during the observation period are between 2.8 cm/s and 13.8 cm/s. The current velocity decreases as the depth increases, and the main current direction is along the northwest. The residual currents in the surface layer of the station are dramatically affected by the local wind, and the southeast wind shifts the residual currents to northwest.

Key words: Tianjin Port, harmonic analysis, tidal currents, residual currents

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