Seasonal variability of the southern tip of the Oxygen Minimum Zone in the eastern South Pacific (30°-38°S): A modeling study

Published in Journal of Geophysical Research: Oceans
Authors

Pizarro-Koch, M, Pizarro, O, Dewitte, B, Montes, I, Ramos, M, Paulmier, A, Garçon V.
Publication year 2019
DOI https://doi.org/10.1029/2019JC015201
Affiliations
  • Programa de Postgrado en Oceanografía, Departamento de Oceanografía, Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Concepción, Chile
  • Millennium Institute of Oceanography, Chile
  • Centrode Investigación Oceanográfica COPAS Sur-Austral, Universidad de Concepción, Chile
  • Department of Geophysics, University of Concepcion, Concepción, Chile
  • Centro de Estudios Avanzados en Zonas Aridas (CEAZA), Coquimbo, Chile
  • Departamento de Biología Marina, Facultad de Ciencias del Mar, Universidad Católica del Norte, Coquimbo, Chile, 
  • Núcleo Milenio de Ecología y Manejo Sustentable de Islas Oceánicas (ESMOI), Universidad Católica del Norte, Coquimbo, Chile
  • LEGOS-CNRS/IRD/UPS/CNES, Toulouse, France
  • Instituto Geofísico del Perú, Lima, Perú
  • Centrode Innovación Acuícola Aquapacífico
IAI Program

CRN3
IAI Project CRN3070
Keywords
eastern South Pacific
oxygen minimum zone
dissolved oxygen

Highlights

•The Oxygen Minimum Zone (OMZ) off Chile is modulated seasonally by the Peru-Chile Undercurrent and by meridionally alternating zonal jets

•Mesoscale eddy Fuxes of dissolvedoxygen (DO), ventilate the OMZ and play a significant, but secondary, role in its seasonal budget

•The advective term is the main driver of the seasonal budget of DO in the OMZ, biogeochemical and mixing processes play a secondary role

Abstract

We investigate the seasonal variability of the southern tip (30°&ndash38°S) of the eastern South Pacific oxygen minimum zone (OMZ) based on a high horizontal resolution (1/12°) regional coupled physical‐biogeochemical model simulation. The simulation is validated by available in situ observations and the OMZ seasonal variability is documented. The model OMZ, bounded by the contour of 45 &muM, occupies a large volume (4.5x104 km3) during the beginning of austral winter and a minimum (3.5x104 km3) at the end of spring, just 1 and 2 months after the southward transport of the Peru‐Chile Undercurrent (PCUC) is maximum and minimum, respectively. We showed that the PCUC significantly impacts the alongshore advection of dissolved oxygen (DO) modulating the OMZ seasonal variability. However, zonal transport of DO by meridionally alternating zonal jets and mesoscale eddy fluxes play also a major role in the seasonal and spatial variability of the OMZ. Consistently, a DO budget analysis reveals a significant contribution of advection terms to the rate of change of DO and the prominence of mesoscale variability within the seasonal cycle of these terms. Biogeochemical processes and horizontal and vertical mixing, associated with subgrid scale processes, play only a secondary role in the OMZ seasonal cycle. Overall, our study illustrates the interplay of mean and (mesoscale) eddy‐induced transports of DO in shaping the OMZ and its seasonal cycle off Central Chile.