On the shape of sea level anomaly signal on periphery of mesoscale ocean eddies
Author:
Affiliation:
1. International Pacific Research Center; SOEST; Honolulu Hawaii USA
2. Now at Instituto Mediterráneo de Estudios Avanzados; Esporles Spain
3. Departament de Fisica; Universitat de les Illes Balears, Edifici Mateu Orfila; Palma Spain
Funder
National Aeronautic and Space Administration (NASA) Physical Oceanography Program
Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
Ministry of Economy and Competitiveness of Spain
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017GL073978/fullpdf
Reference17 articles.
1. Coherent mesoscale eddies in the North Atlantic subtropical gyre: 3-D structure and transport with application to the salinity maximum;Amores;J. Geophys. Res. Oceans,2017
2. Archiving, Validation, and Interpretation of Satellite Oceanographic data 2016 SSALTO/DUACS user handbook: (M)SLA and (M)ADT near-real time and delayed time products
3. Vertical structure of mesoscale eddies in the eastern South Pacific Ocean: A composite analysis from altimetry and Argo profiling floats;Chaigneau;J. Geophys. Res.,2011
4. Global observations of nonlinear mesoscale eddies;Chelton;Progr. Oceanogr.,2011
5. Routes of Agulhas rings in the southeastern Cape Basin;Dencausse;Deep Sea Res., Part I,2010
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