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Poleward Flows Along Eastern Ocean Boundaries

  • S. J. Neshyba
  • Ch. N. K. Mooers
  • R. L. Smith
  • R. T. Barber

Part of the Coastal and Estuarine Studies book series (COASTAL, volume 34)

Table of contents

  1. Front Matter
    Pages I-IX
  2. Workshop Summaries

  3. Geographical Reports

    1. Front Matter
      Pages 45-45
    2. The Atlantic Ocean

    3. The Pacific Ocean

      1. Adriana Huyer, P. Michael Kosro, Steven J. Lentz, Robert C. Beardsley
        Pages 142-159
      2. A. Badan-Dangon, J. M. Robles, J. García
        Pages 176-202
    4. The Indian Ocean

      1. John A. Church, George R. Cresswell, J. Stuart Godfrey
        Pages 230-254
  4. Special Topics

  5. Epilogue

    1. Front Matter
      Pages 331-331
    2. S. J. Neshyba, Ch. N. K. Mooers, R. L. Smith, R. T. Barber
      Pages 332-341
  6. References

    1. Front Matter
      Pages 342-342
    2. S. J. Neshyba, Ch. N. K. Mooers, R. L. Smith, R. T. Barber
      Pages 343-370
  7. Back Matter
    Pages 371-377

About this book

Introduction

In this paper differences and anomalies in west coast seasonal flow structures have been highlighted. In particular, it was emphasized that flow off Washington has significant differences from that of Oregon; namely, during summer, flow at mid-shelf is more poleward off Washington, and during winter, flow on the inner-shelf is more equatorward off Washington than off Oregon. The former result may be related to the poleward decrease in the longshelf wind stress; the latter result may be related to the presence of the Columbia River plume. Off southern California the near-surface flow over the shelf is more persistently equatorward than that off Washington . Conversely, the flow over the slope in the upper 100 m of the water column is more persistently poleward than that off washington. Also, the undercurrent structure, that is, a subsurface maximum, is maintained at least from summer to early winter off southern California (no data are yet available from spring), but only during summer and early fall off washington. We note that the seasonal cycle of vertical shear in the two locations is similar, although a reversal in sign sometimes occurs off Washington. ACKNOWLEDGEMZNTS This work was supported by the Department of Energy under Grant DE-FG05-85ER60333t4 and by the National Science Foundation under Grant OCE 86-01058#1. 175 From: Adriana Huyer, College of Oceanography, Oregon State University, Corvallis, OR. On: Review and Commentary to paper POLEWARD FLOW NEAR TRE NORTRERH AND SOU'l'BERH BOONDARIES OF TRE U. S. WEST COAST, by Barbara Hickey.

Keywords

Atlantic Ocean Coast Indian Ocean Meere Meeresbiologie Ozeanographie Pacific Ocean biology marine biology nitrogen ocean oceanography

Editors and affiliations

  • S. J. Neshyba
    • 1
  • Ch. N. K. Mooers
    • 2
  • R. L. Smith
    • 1
  • R. T. Barber
    • 3
  1. 1.College of OceanographyOregon State UniversityCorvallisUSA
  2. 2.Institute for Naval OceanographyStennis Space CenterUSA
  3. 3.Monterey Bay Aquarium Research InstitutePacific GroveUSA

Bibliographic information

  • DOI https://doi.org/10.1007/978-1-4613-8963-7
  • Copyright Information Springer-Verlag New York 1989
  • Publisher Name Springer, New York, NY
  • eBook Packages Springer Book Archive
  • Print ISBN 978-1-4613-8965-1
  • Online ISBN 978-1-4613-8963-7
  • Series Print ISSN 0724-5890
  • Buy this book on publisher's site