ArticlePhilosophical transactions. Series A, Mathematical, physical, and engineering sciences2017
Ocean (de)oxygenation from the Last Glacial Maximum to the twenty-first century: insights from Earth System models.
Article in Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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Who cites it
5 citing papers in PubMed, 92 citations in OpenAlex.
- North Atlantic ventilation change over the past three decades is potentially driven by climate change.Nature communications · 2026Article
- Short-term focus: phased response of Zostera marina seedlings to the combined stress of marine heatwave and ocean acidification.BMC plant biology · 2025Article
- Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points.Surveys in geophysics · 2025Review
- Article
- Ocean ventilation and deoxygenation in a warming world: introduction and overview.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2017Article
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Authors and funding
5 authors at 3 institutions in 2 countries.
Funding
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Abstract
All Earth System models project a consistent decrease in the oxygen content of oceans for the coming decades because of ocean warming, reduced ventilation and increased stratification. But large uncertainties for these future projections of ocean deoxygenation remain for the subsurface tropical oceans where the major oxygen minimum zones are located. Here, we combine global warming projections, model-based estimates of natural short-term variability, as well as data and model estimates of the Last Glacial Maximum (LGM) ocean oxygenation to gain some insights into the major mechanisms of oxygenation changes across these different time scales. We show that the primary uncertainty on future ocean deoxygenation in the subsurface tropical oceans is in fact controlled by a robust compensation between decreasing oxygen saturation (O
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