View Item 
        •   Utrecht University Student Theses Repository Home
        • UU Theses Repository
        • Theses
        • View Item
        •   Utrecht University Student Theses Repository Home
        • UU Theses Repository
        • Theses
        • View Item
        JavaScript is disabled for your browser. Some features of this site may not work without it.

        Browse

        All of UU Student Theses RepositoryBy Issue DateAuthorsTitlesSubjectsThis CollectionBy Issue DateAuthorsTitlesSubjects

        Analysis of nontraditional Coriolis terms on linear equatorial shallow water model and boundary layers

        Thumbnail
        View/Open
        Final draft.pdf (1.423Mb)
        Publication date
        2021
        Author
        Liu, H.
        Metadata
        Show full item record
        Summary
        The equatorial region is treated as a boundary layer in this study and analysed in numerical and analytical perspectives. A simple numerical equatorial dynamic model based on Zebiak and Cane’s model (ZC model) is developed in this study. Though the model contains ocean-atmosphere coupled processes, it is found that the surface layer requires a more detailed description as a singularity occurs at the equator. Dimensional analysis suggests that nontraditional Coriolis force terms and meridional diffusion terms are not negligible in the equatorial region. In consequence boundary layers occur both in meridional direction near the equator and in vertical direction, near the surface. Using matched asymptotic expansion, we conclude that the outer solutions of the problem follows parabolic characteristics. An attempt to find the inner solutions in both boundary layers (excluding overlapping region) is also presented in this study. Through the discussion of these solutions, we show that the outer solutions originate from the surface boundary layer forced by surface wind stress in both hemispheres, develop in the form of parabolic characteristics, and converge at the equator through meridionally-oriented equatorial boundary layer. The equatorial boundary layer is a transition zone that connects both hemispheres, and the vertical structure within the equatorial boundary layer is related directly with the wind stress and the meridional pressure gradient at the surface in off-equator region.
        URI
        https://studenttheses.uu.nl/handle/20.500.12932/40942
        Collections
        • Theses
        Utrecht university logo