Journal of Oceanography

, Volume 60, Issue 2, pp 365–374 | Cite as

Monitoring Surface Velocity from Repeated ADCP Observations and Satellite Altimetry

  • Kaoru Ichikawa
  • Noriaki Gohda
  • Masazumi Arai
  • Arata Kaneko


A method has been developed to monitor the surface velocity field by combining repeated acoustic Doppler current profiler (ADCP) observations and satellite altimetry data. The geostrophic velocity anomaly is calculated from the sea surface height anomaly field estimated from the altimetry data by an optimal interpolation. It has been confirmed that this accurately observes the smoothed velocity anomaly field when the interpolation scales are set according to the spatio-temporal sampling pattern of the altimeter used. The velocity anomaly obtained from the altimetry data is subtracted from the repeated ADCP observations to estimate temporal mean velocity along the ship tracks. Regularly sampled, nine-year time series of surface velocity can then be obtained by adding the computed mean velocity and the altimetry anomaly components. This clearly illustrates surface velocity fluctuations such as the movement of the Kuroshio axis due to its meandering and an increase of the interannual variability of the Subtropical Countercurrent toward its downstream region.

ADCP altimeter surface velocity Kuroshio Subtropical Countercurrent 


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Copyright information

© The Oceanographic Society of Japan 2004

Authors and Affiliations

  • Kaoru Ichikawa
    • 1
    • 2
  • Noriaki Gohda
    • 3
  • Masazumi Arai
    • 3
  • Arata Kaneko
    • 3
  1. 1.Research Institute for Applied MechanicsKyushu UniversityFukuokaJapan
  2. 2.Frontier Observational Research System for Global ChangeKanagawaJapan
  3. 3.Division of Global Environment Engineering, Graduate School of EngineeringHiroshima UniversityHigashi-HiroshimaJapan

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