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Projected Future of African Marine Ecosystems Under Climate Change and Stratospheric Aerosol Injection

  • Founi M. Awo
  • , Babatunde J. Abiodun
  • , Isabelle Ansorge
  • , Folly S. Tomety
  • , Djoirka M. Dimoune
  • , Annette Samuelsen
  • , Daniele Visioni
  • , Marek Ostrowski
  • , Simone Tilmes
  • Université de San-Pédro
  • University of Cape Town
  • Université Nationale des Sciences
  • Nansen Environmental and Remote Sensing Center
  • Cornell University
  • Institute of Marine Research

Research output: Contribution to journalArticlepeer-review

Abstract

Stratospheric Aerosol Injection (SAI) has been proposed as a potential strategy to cool the planet. The ARISE-SAI-1.5 approach, which employes a moderate emission scenario, is simulated to limit future global warming to 1.5°C by injecting aerosols into the stratosphere in the year 2035. However, the climate response to this SAI scenario, particularly along the African coast, remains unclear. In this study, we investigate the potential impacts of climate change under the SSP2-4.5 scenario and ARISE-SAI-1.5 on regional African marine ecosystems through key biological (chlorophyll), physical (salinity, temperature), and chemical (nitrate, acidification, and dissolved oxygen) parameters. Our results indicate that climate change may reduce productivity in African coastal ecosystems, with chlorophyll concentrations decreasing between 10% and 62%. Sea surface temperatures are projected to rise by 1.5°C along the entire coast by 2069, while surface salinity increases up to 0.3 g/kg, except for a slight decrease of up to 0.1 g/kg along the Congolese-Angolan coast. This salinity dipole in the Gulf of Guinea results from enhanced precipitation and river discharge, reinforced by stratification that traps freshwater at the surface. Additionally, climate change drives ocean acidification and may expand the oxygen minimum zone in the Gulf of Guinea, with oxygen levels decreasing by 10%–30% at depths of 100–200 m. Although ARISE-SAI-1.5 may help reduce surface oxygen depletion, it may not significantly mitigate subsurface oxygen loss or continued acidification. Nevertheless, it may reduce some negative climate change impacts on marine ecosystems by stabilizing chlorophyll levels, sea surface temperatures, and salinity.

Original languageEnglish
Article numbere2025JC022687
JournalJournal of Geophysical Research: Oceans
Volume131
Issue number5
DOIs
StatePublished - May 2026

Keywords

  • ARISE-SAI-1.5
  • chlorophyll concentration
  • climate change
  • dissolved oxygen
  • marine ecosystem
  • river discharge

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