Observation of the abyssal current in the West Mariana Basin

  • Noriya Yoshioka
  • Masahiro Endoh
  • Hiroshi Ishizaki


In order to investigate long-term variations of deep sea currents and temperature in the western North Pacific, a direct current measurement was made at 12.5°N, 137°E from July 1985 to July 1986. The current meter was moored at a depth of about 4,000 m (bottom depth 4,604 m) in the West Mariana Basin, very close to the deep water passage to the North Pacific Basin. Throughout the observed period, the current flows southward with an average speed of 0.8 cm sec−1. There are significant variations of both currents and temperature within the period of 60 days. For the shorter time scales, in addition to the tidal oscillations with one day and half day periods, there is a notable spectral peak of the current with a clockwise rotation at a period of 2.2 days, which is slightly shorter than the local inertial period of 2.3 days.

The observed southward current seems to indicate that the deep sea water in the West Mariana Basin flows out through the sill which is deeper than 4,000 m and is located about 200 km southeast of the mooring point. A simple analysis of the linear plane wave indicates that the medium time-scale variation with a period of 60 days is associated with the barotropic Rossby wave whose wavelength is 390 km and whose trough direction is 30° clockwise from the north.


Rossby Wave Clockwise Rotation Pacific Basin Bottom Depth Water Passage 
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Copyright information

© Oceanographical Society of Japan 1987

Authors and Affiliations

  • Noriya Yoshioka
    • 1
  • Masahiro Endoh
    • 1
  • Hiroshi Ishizaki
    • 1
  1. 1.Meteorological Research InstituteTsukubaJapan

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