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Volume 44 Issue 5
Jun.  2022
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Article Contents
Kuang Fangfang,Zhang Junpeng,Zhou Xiwu, et al. Low frequency variation of deep current at Niulang Seamount based on submarine mooring observation[J]. Haiyang Xuebao,2022, 44(5):71–79 doi: 10.12284/hyxb2022085
Citation: Kuang Fangfang,Zhang Junpeng,Zhou Xiwu, et al. Low frequency variation of deep current at Niulang Seamount based on submarine mooring observation[J]. Haiyang Xuebao,2022, 44(5):71–79 doi: 10.12284/hyxb2022085

Low frequency variation of deep current at Niulang Seamount based on submarine mooring observation

doi: 10.12284/hyxb2022085
  • Received Date: 2021-08-18
  • Rev Recd Date: 2021-11-17
  • Available Online: 2022-06-17
  • Publish Date: 2022-06-15
  • Based on the long-term observation obtained from two sets of submarine mooring system deployed at Niulang Seamount in the western Pacific, the vertical distribution of the deep currents and the temporal variation characteristics were analyzed in the paper. The results show that: (1) The annual mean ocean currents and the variations were the largest in the upper layer, the second in the middle and deep layers, and the smallest in the middle-deep layers. (2) The subtropical countercurrent was at the depth shallower than 150 m, and the northward current was at depth deeper than 150 m and at the middle layers; the near bottom current was weak southward at the summit of the seamount, but southwestward at the bottom of the seamount. (3) Both at the summit and bottom of the seamount, the currents showed a seasonal oscillation with the most energetic oscillation at a period of about 100 d throughout the water column; at depth above 2 000 m, currents showed a synchronous oscillation in the throughout the water column, with the oscillation amplitude decreasing with depth; current oscillation at deep layers (below 2 000 m) were in opposite phase with that at the upper layers, and the oscillation amplitude was the strongest at 4 000 m.
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