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Numerical modelling of the ocean circulation in the Canadian Arctic Archipelago

  • Author / Creator
    Wang, Qiang
  • The Canadian Arctic Archipelago (CAA) is a complex network of straits and
    basins connecting the Arctic Ocean and the Atlantic Ocean. It is one of the
    main pathways for freshwater outflow from the Arctic Ocean to the Atlantic
    Ocean. Circulation and associated variability in the CAA are examined in this
    thesis using numerical models.
    After correcting for shortwave radiation, the CAA model captures much of
    the observed spatiotemporal structure of the sea ice and ocean circulation in
    the Canadian Arctic Archipelago, especially, the southward flow in M’Clintock
    Channel and cyclonic circulation in eastern Lancaster Sound. The momentum
    balance of ocean currents is studied and we found that the southward flow in
    M’Clintock Channel is driven by ageostrophic accelerations and is controlled
    by topography. Vorticity dynamics analysis shows that both stratification
    and bathymetry have a strong impact on the circulation in eastern Lancaster
    Sound.
    We did some sensitivity experiments to study the impact of the stress on the
    volume transport through Lancaster Sound and Nares Strait. We found that
    the ice stress on the ocean in Parry Channel has a strong impact on the seasonal
    variation of volume transport through Lancaster Sound. The boundary flows
    also have a strong impact on the volume transport through Lanaster Sound
    and Nares Striat. The ice stress on the ocean in Parry Channel, stress on the
    ocean in Nares Strait, stress on the ocean in Baffin Bay all have an impact on
    the seasonal variation of volume transport through Nares Strait.

  • Subjects / Keywords
  • Graduation date
    Fall 2012
  • Type of Item
    Thesis
  • Degree
    Doctor of Philosophy
  • DOI
    https://doi.org/10.7939/R3T66N
  • License
    This thesis is made available by the University of Alberta Libraries with permission of the copyright owner solely for non-commercial purposes. This thesis, or any portion thereof, may not otherwise be copied or reproduced without the written consent of the copyright owner, except to the extent permitted by Canadian copyright law.
  • Language
    English
  • Institution
    University of Alberta
  • Degree level
    Doctoral
  • Department
  • Supervisor / co-supervisor and their department(s)
  • Examining committee members and their departments
    • Christian Haas (University of Alberta, Earth and Atmospheric Sciences),
    • Yves Gratton (University of Québec Institut National de la Recherche Scientifique)
    • Vincent L St. Louis (Univ. of Alberta, Biological Sciences)