Tide and current observations in the central Chukchi Sea during the summer of 2012
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  • 作者:Huiwu Wang ; Na Liu ; Hongxia Chen
  • 关键词:central Chukchi Sea ; tidal and residual currents ; local wind forcing
  • 刊名:Journal of Ocean University of China
  • 出版年:2016
  • 出版时间:April 2016
  • 年:2016
  • 卷:15
  • 期:2
  • 页码:201-208
  • 全文大小:753 KB
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  • 作者单位:Huiwu Wang (1) (2)
    Na Liu (2)
    Hongxia Chen (2)

    1. College of Physical and Environmental Oceanography, Ocean University of China, Qingdao, 266100, P. R. China
    2. First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, P. R. China
  • 刊物主题:Oceanography; Meteorology;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1993-5021
文摘
Current data from a moored Acoustic Doppler Current Profiler (ADCP) deployed at 69°30.155´N, 169°00.654´W in the central Chukchi Sea during 2012 summertime is analyzed in the present paper. Characteristics of tidal and residual currents are obtained with Cosine-Lanczos filter and cross-spectral analyses. The main achievements are as follows: 1) Along with the local inertial frequency of 12.8 h, two other peaks at ~12-h and ~10-d dominate the time series of raw velocity; 2) The M2 dominates the 6 resolved tide constituents with significant amplitude variations over depth and the ratios of current speed of this constituent to that of the total tidal current are 54% and 47% for u and v components, respectively. All the resolved tidal constituents rotate clockwise at depth with the exception of MM and O1. The constituents of M2 and S2 with the largest major semi-axes are similar in eccentricity and orientation at deeper levels; 3) The maximum of residual currents varies in a range of 20–30 cm s−1 over depth and the current with lower velocities flow more true north with smaller magnitudes compared to the current in surface layer. The ~10 d fluctuation of residual current is found throughout the water column and attributed to the response of current to the local wind forcing, with an approximate 1.4 d lag-time at the surface level and occurring several hours later in the lower layer; 4) Mean residual currents flow toward the north with the magnitudes smaller than 7 cm s−1 in a general agreement with previous studies, which suggests a relatively weaker but stable northward flow indeed exists in the central Chukchi Sea. Keywords central Chukchi Sea tidal and residual currents local wind forcing

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