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• W3136384281 abstract "Abstract Less than a quarter of ocean deoxygenation that will ultimately be caused by historical CO 2 emissions is already realized, according to millennial-scale model simulations that assume zero CO 2 emissions from year 2021 onwards. About 80% of the committed oxygen loss occurs below 2000 m depth, where a more sluggish overturning circulation will increase water residence times and accumulation of respiratory oxygen demand. According to the model results, the deep ocean will thereby lose more than 10% of its pre-industrial oxygen content even if CO 2 emissions and thus global warming were stopped today. In the surface layer, however, the ongoing deoxygenation will largely stop once CO 2 emissions are stopped. Accounting for the joint effects of committed oxygen loss and ocean warming, metabolic viability representative for marine animals declines by up to 25% over large regions of the deep ocean, posing an unavoidable escalation of anthropogenic pressure on deep-ocean ecosystems." @default.
• W3136384281 created "2021-03-29" @default.
• W3136384281 creator A5063745149 @default.
• W3136384281 date "2021-04-16" @default.
• W3136384281 modified "2023-09-26" @default.
• W3136384281 title "A committed fourfold increase in ocean oxygen loss" @default.
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• W3136384281 doi "https://doi.org/10.1038/s41467-021-22584-4" @default.
• W3136384281 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/8052459" @default.
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• W3136384281 hasPublicationYear "2021" @default.
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