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Mesoscale Eddy Properties in Four Major Western Boundary Current Regions

Oceanic mesoscale eddies are a kind of typical geostrophic dynamic process which can cause vertical movement in water bodies, thereby changing the temperature, salinity, density, and chlorophyll concentration of the surface water in the eddy. Based on multisource remote sensing data and Argo profile...

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Autors principals: Wei Cui, Jungang Yang, Chaojie Zhou
Format: Artigo
Idioma:Inglês
Publicat: MDPI AG 2024-11-01
Col·lecció:Remote Sensing
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Accés en línia:https://www.mdpi.com/2072-4292/16/23/4470
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