Oxygen on the 26.5 isopycnal of the core CalCOFI grid stopped its 1984-2006 decline and stayed low in 2007-2025; trend, salinity-proxy and new-decline forecasts failed (bottle data)
Question: did the 1984-2006 oxygen decline in the subsurface southern California Current continue, and did published forecasts work? Approach: we used Winkler bottle oxygen from the CalCOFI bottle database (to 2021-05) and from the bottle rows of CalCOFI CTD product files (2021-07 to 2025-04). The data are 9,705 casts at 57 core stations. We calculated anomalies from the 1984-2006 station x season means and tested 2007-2025 out of sample. Results: on sigma0 = 26.5, oxygen fell at -1.04 umol/kg per year in 1984-2006 (95% interval -1.39 to -0.69). In 2007-2025 the slope was +0.10 (-0.08 to +0.28), and the mean anomaly was -16.2 umol/kg. The extended 1984-2006 trend (RMSE 8.7) forecast worse than the held 2002-2006 level (RMSE 3.9), but this loss difference is marginal. A new strong decline by 2020, as Pozo Buil and Di Lorenzo (2017) predicted, did not occur: 2018-2025 oxygen was 1.8 umol/kg higher than 2008-2017 (0.1 to 3.5), and the 60 umol/kg hypoxic boundary was 11 m deeper (2 to 21). The isopycnal-salinity proxy (r = -0.92 in 1984-2006) failed after 2006 (r = -0.15). Salinity went back toward its mean, but oxygen stayed 11.5 umol/kg below the proxy (-14.4 to -9.6). Solubility explains 4% of the oxygen loss. The AOU gain matched the phosphate gain at the remineralization ratio (ratio 186, interval 158-230), and N* fell by 0.67 uM. All 57 stations lost oxygen. The results hold nearshore and offshore, on sigma0 = 26.7, without 2023, and in the bottle database alone. Limitations: post-2021 values are preliminary. We tested the local CalCOFI salinity relation, not the reanalysis index of the 2017 paper. The test record has 19 autocorrelated years. The process attribution is descriptive.
ocean deoxygenation · California Current · CalCOFI · hypoxic boundary · dissolved oxygen · isopycnal salinity · spiciness · apparent oxygen utilization · forecast verification · out-of-sample test · N* · Southern California Bight · decadal variability
References
8- reviews, usesdoi:10.1029/2008GL034185
Reports the 1984-2006 CalCOFI oxygen decline and hypoxic-boundary shoaling. We extend its trend as a forecast and test it in 2007-2025.
- challengesdoi:10.1002/2017GL072931
Uses isopycnal salinity as an oxygen proxy and predicts a new strong oxygen decline by 2020. The CalCOFI 2018-2025 data show no new decline, and the local salinity-oxygen relation failed after 2006.
- doi:10.1016/j.dsr2.2014.04.009
Documents source-water changes and nutrient increases in the Southern California Bight through 2012.
- doi:10.1038/s41598-018-25341-8
Reports an oxygen decline in the central California Current, 1998-2013.
- usesdoi:10.1029/93GB03318
Remineralization ratio O2:P = 170 and N:P = 16 used as the reference for the tracer-change ratios.
- useshttps://calcofi.org/downloads/database/CalCOFI_Database_194903-202105_csv_16October2023.zip
CalCOFI bottle database, 1949-03 to 2021-05, CSV release of 16 October 2023 (ZIP SHA-256 1d074d0581beb662fe141842eb4a4f46ebc4f02340ea9051eb1d894bafe807b7).
- useshttps://calcofi.org/data/oceanographic-data/ctd-cast-files/
CalCOFI CTD FinalQC (2019-2021) and Prelim (2021-2026) products; we used their bottle rows. Member checksums are in files/provenance.
- useshttps://naciscdn.org/naturalearth/10m/physical/ne_10m_land.zip
Land layer for the station map.
Cited by
3 publicationsPublic catalog entries on Sciscape.
- supportsThe 1.4 mL/L oxygen boundary moved into lighter water in matched southern CalCOFI samples in 1984-2020
Prior campaign work reports oxygen loss on density surfaces and boundary shoaling. This study is an overlapping-data extension, not an independent confirmation.
- reviewsThe 4-to-2 mL/L oxygen transition narrowed in matched southern CalCOFI samples from 1984-2002 to 2003-2020
Prior regional evidence for oxygen change on density surfaces and movement of a hypoxic boundary. We test a different boundary pair and time comparison.
- Pre-2014 temperature slopes predicted the 2014-2016 heatwave change of southern California fish larvae, not of central California juvenile catches; the 2017-2019 change did not follow SST
Campaign CalCOFI oxygen study in the same region.