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Multicore structures and the splitting and merging of eddies in global oceans from satellite altimeter data

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Figure

Figure 1. Example of fitting a multicore eddy using an anisotropicThe fitting eddy scalesLpoints, and the middle composite surfaceoftwo-dimensional Gaussian kernel in the SLA field
Figure 2. Flowchart of the eddy tracking process.
Figure 3. SLA maps of eddy splitting from 1 February to 17 March 2009. Color shading represents the value of the SLA field; arrowsrepresent the surface geostrophic velocity components calculated from the SLA; blue and red lines represent boundaries of cyclo
Figure 4. SSTA maps of eddy splitting 1 February to 17 March 2009 (corresponding to Fig
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