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Ocean Science An interactive open-access journal of the European Geosciences Union
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OS | Articles | Volume 14, issue 1
Ocean Sci., 14, 69–86, 2018
https://doi.org/10.5194/os-14-69-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Ocean Sci., 14, 69–86, 2018
https://doi.org/10.5194/os-14-69-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 02 Feb 2018

Research article | 02 Feb 2018

Response of O2 and pH to ENSO in the California Current System in a high-resolution global climate model

Giuliana Turi et al.
Data sets

The NCEP/NCAR 40-year reanalysis project (https://www.esrl.noaa.gov/psd/data/gridded/) E. Kalnay, M. Kanamitsu, R. Kistler, W. Collins, D. Deaven, L. Gandin, M. Iredell, S. Saha, G. White, J. Woollen, Y. Zhu, A. Leetmaa, R. Reynolds, M. Chelliah, W. Ebisuzaki, W. Higgins, J. Janowiak, K. C. Mo, C. Ropelewski, J. Wang, R. Jenne, and D. Joseph https://doi.org/10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2

Sea-viewing Wide Field-of-view Sensor (SeaWiFS) Ocean Color Data, 2014 Reprocessing NASA, Goddard Space Flight Center, Ocean Ecology Laboratory, Ocean Biology Processing Group https://doi.org/10.5067/ORBVIEW-2/SEAWIFS_OC.2014.0

An historical analysis of the California Current circulation using ROMS 4D-Var: System configuration and diagnostics (http://oceanmodeling.ucsc.edu) E. Neveu, A. M. Moore, C. A. Edwards, J. Fiechter, P. Drake, W. J. Crawford, M. G. Jacox, and E. Nuss https://doi.org/10.1016/j.ocemod.2015.11.012

Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century (http://www.metoffice.gov.uk/hadobs/hadisst/) N. A. Rayner, D. E. Parker, E. B. Horton, C. K. Folland, L. V. Alexander, D. P. Rowell, E. C. Kent, and A. Kaplan https://doi.org/10.1029/2002JD002670

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Short summary
A high-resolution global model was used to study the influence of El Niño/La Niña events on the California Current System (CalCS). The mean surface oxygen (O2) response extends well offshore, where the pH response occurs within ~ 100 km of the coast. The surface O2 (pH) is primarily driven by temperature (upwelling) changes. Below 100 m, anomalously low O2 and low pH occurred during La Niña events near the coast, potentially stressing the ecosystem, but there are large variations between events.
A high-resolution global model was used to study the influence of El Niño/La Niña events on...
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