Articles | Volume 19, issue 2
https://doi.org/10.5194/os-19-351-2023
https://doi.org/10.5194/os-19-351-2023
Research article
 | 
30 Mar 2023
Research article |  | 30 Mar 2023

The signature of NAO and EA climate patterns on the vertical structure of the Canary Current upwelling system

Tina Georg, Maria C. Neves, and Paulo Relvas

Data sets

CMEMS: Global Ocean Ensemble Physics Reanalysis (PHY\_001\_026) E.U. Copernicus Marine Service Information https://doi.org/10.48670/moi-00023

ERA5 monthly averaged data on single levels from 1959 to present H. Hersbach, B. Bell, P. Berrisford, G. Biavati, A. Horányi, J, Muñoz Sabater, J. Nicolas, C. Peubey, R. Radu, I. Rozum, D. Schepers, A. Simmons, C. Soci, D. Dee, and J.-N. Thépaut https://doi.org/10.24381/cds.f17050d7

National Weather Service, Climate Prediction Center NOAA https://www.cpc.ncep.noaa.gov/data/teledoc/ea.shtml

National Weather Service, Climate Prediction Center: North Atlantic Oscillation (NAO) NOAA https://www.cpc.ncep.noaa.gov/products/precip/CWlink/pna/nao.shtml

Environmental Research Division NOAA Fisheries https://oceanview.pfeg.noaa.gov/products/upwelling/bakun

Download
Short summary
This study aims to analyse the changes of the vertical structure of the ocean during upwelling and the role of climate patterns in the Canary Current (25–35°N) over a period of 25 years (1993–2017). Ocean mixing is enhanced during upwelling events and extends deeper (shallower) in the winters of positive (negative) North Atlantic Oscillation. It is enhanced during coupled, opposite phases of the East Atlantic pattern, suggesting stronger upwelling activity independent of climate patterns.