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Lagrangian Mesoscale Eddy Evolution in the Western Arabian Sea: Comparing Surface Temperature Anomaly with Vertical Structure
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How Atmospheric Forcing Frequency, Horizontal and Vertical Grid Resolutions Impact Mesoscale Eddy Evolution in a Numerical Model
1 Introduction Mesoscale eddies are ubiquitous turbulent structures in the oceans, in thermal wind balance with a signature in density: positive density anomaly for an anticyclone, respectively negative for a cyclone.
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