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Title: Near-inertial motions over a mid-ocean ridge: Effects of topography and hydrothermal plumes

Journal Article · · Journal of Geophysical Research; (United States)
 [1]; ;  [2]
  1. Inst. of Ocean Sciences, Sidney, British Columbia (Canada)
  2. Oregon State Univ., Corvallis (United States)

The authors investigate the spatial structure of near-inertial motions in the vicinity of the Endeavour segment of Juan de Fuca Ridge (approximately 48{degree}N, 129{degree}W) in the northeast Pacific Ocean. Within the lower 1,000 m of the water column where most of the observations were obtained, near-inertial oscillations have rms current speeds of O(1 cm/s) and vertical isotherm displacements of O(10 m). The fluctuations are confined to the frequency band 0.966-1.079 f (f is the local Coriolos parameter) and have characteristic event durations of 1 week. Marked alteration of the near-inertial current amplitudes occurs over two well-defined depth zones within the study region. Within the 200-m zone immediately above the 2,100-m ridge crest, current amplitudes are amplified by a factor of 1.2-1.7 because of bottom reflection and/or scattering of the downward propagating energy. Evidence that the amplification may be linked to bottom reflection rather than to scattering is provided by flattening and cross-slope rotation of the near-inertial current ellipses with increased proximity to the top of the ridge. Near-inertial motions are estimated to have vertical coherence scales of the order of 10-100 m, while horizontal coherence scales exceed the 50-km separation between the mooring locations. Minimum vertical and horizontal coherences are found for the depth zone 1,600-1,800 m, while maximum correlation occurs for near-bottom motions immediately above the crest of the ridge. Weak near-inertial motions are observed within the 100-m-deep axial valley.

OSTI ID:
5009654
Journal Information:
Journal of Geophysical Research; (United States), Vol. 95:C5; ISSN 0148-0227
Country of Publication:
United States
Language:
English