A Geometric Framework for Mapping Ocean Eddies Using Elliptical Streamfunction Parameterisation
Abstract. The identification, tracking, and characterisation of ocean eddies using observational and numerical data is essential for understanding eddy dynamics and their global climate impacts. Eulerian (point-based) and Lagrangian (trajectory-based) schemes are widely used to detect and track ocean eddies. However, these methods typically do not provide information about the spatial structure of eddies or properties such as vorticity, deformation, and vertical tilt, especially when using sparse data. Here, we describe a new efficient and robust geometrical approach for mapping the three dimensional structure of ocean eddies by fitting (partial) velocity data to a simplified elliptical streamfunction model with a small number of parameters. The flexibility of the approach is demonstrated through three variants of the method adapted to different velocity sampling patterns: single and double sections (from ship transects or a numerical grid) and scattered data (e.g. from surface drifters). We validate and demonstrate these new geometric methods on idealised, axisymmetric and non-axisymmetric Gaussian eddies, as well as numerical and observational datasets. We conclude that elliptical streamfunction parametrisation offers a versatile and effective method for research into ocean eddy characteristics.
A Geometric Framework for Mapping Ocean Eddies Using Elliptical Streamfunction Parameterisation
The present study uses the elliptical streamfunction parameterization method to determine the vorticity, deformation and vertical tilt of the mesoscale eddies. The employment of this methodology enables the delineation of the eddy geometric structure for both single and double sections, through the utilization of a minimal number of parameters for the alignment of velocity data. The present study is timely and of interest. The importance of the eddy asymmetric structures (e.g., horizontal deformation and vertical tilt) has been noticed in recent years. The present study is capable of providing a theoretical description of the eddy asymmetric structures by limited observations. I recommended that a minor revision be undertaken before the text can be considered acceptable.
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References
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