The 3‐D Structure of Mesoscale Eddies in the Lofoten Basin of the Norwegian Sea: A Composite Analysis From Altimetry and In Situ Data

Author:

Sandalyuk Nikita V.1ORCID,Bosse Anthony23ORCID,Belonenko Tatyana V.1

Affiliation:

1. Department of Oceanology Saint Petersburg State University Saint Petersburg Russia

2. Geophysical Institute University of Bergen and Bjerknes Center for Climate Research Bergen Norway

3. Now at Aix‐Marseille Univ., Université de Toulon, CNRS, IRD, MIO UM Marseille France

Funder

Norges Forskningsråd

Russian Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference73 articles.

1. Structure and circulation of water masses in the area of an anticyclonic vortex in the north‐eastern part of the Norwegian Sea;Alexeev G. V.;Russian problems of Arctic and Antarctic,1991

2. Amante C. &Eakins B. W.(2009).ETOPO1 1 Arc‐Minute Global Relief Model: Procedures data sources and analysis. NOAA Technical Memorandum NESDIS NGDC‐24. National Geophysical Data Center NOAA.https://doi.org/10.7289/V5C8276M

3. Variability of the Norwegian Atlantic Current and associated eddy field from surface drifters

4. Argo(2020).Argo float data and metadata from Global Data Assembly Centre (Argo GDAC). SEANOE.http://doi.org/10.17882/42182

5. Quantifying the influence of Atlantic heat on Barents Sea ice variability and retreat;Årthun M.;Journal of Climate,2012

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