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The response of the ocean carbon cycle to artificial upwelling, ocean iron fertilization and the combination of both

Bibliographic Data

ID15545351
AuthorsMalte Jürchott (0000-0002-5236-3108, GEOMAR Helmholtz Centre for Ocean Research Kiel, corresponding author), Wolfgang Koeve (0000-0002-2298-9230, GEOMAR Helmholtz Centre for Ocean Research Kiel), Andreas Oschlies (0000-0002-8295-4013, Christian-Albrechts-Universität zu Kiel)
Year2024
Volume19
Issue11
Pages114088-114088
Publication date2024-10-10
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ad858d
OpenAlexW4403289144
LanguageEN
Citations received3
References cited42

Artificial upwelling (AU) and ocean iron fertilization (OIF) both have been proposed as marine carbon dioxide removal methods to enhance ocean carbon uptake by stimulating the biological carbon pump. We simulate global and regional AU and OIF individually and the combination of both methods between the years 2025 and 2100 in ocean-atmosphere model experiments under the moderate RCP 4.5 CO 2 -emission pathway and show that the combination of globally applied AU + OIF yields the greatest ocean carbon uptake potential of +103 Pg C until year 2100. Regional OIF simulated by itself poleward of 45° North and South is responsible for +86.9 Pg C additional ocean carbon uptake. AU-only experiments do not significantly enhance ocean carbon uptake due to the lack of iron in the upwelled waters. We find no consistent relationship between enhanced cumulative export production and changes in the ocean carbon inventory attributable to the biological carbon pump, which makes export production a poor indicator for additional ocean carbon uptake. We identified a strong decrease in the global ocean nitrate inventory (−567 Tmol N) until year 2100 as a consequence of globally applied AU + OIF due to an interrupted balance between N 2 -fixation and denitrification

Biological pump · Biology · Carbon cycle · Carbon dioxide · Carbon fibers · Carbon sequestration · Denitrification · Ecosystem · Iron fertilization · Nitrate · Nitrogen · Nutrient · Phytoplankton · Primary production · Total inorganic carbon · Total organic carbon · Upwelling · Chemistry · Environmental Science · Marine and coastal ecosystems · Materials Science · Methane Hydrates and Related Phenomena · Ocean Acidification Effects and Responses · Ecology · Environmental Chemistry · Geology · Oceanography

  • Potential impacts of marine carbon dioxide removal on ocean oxygen

    Open Access•Andreas Oschlies, C P Slomp et al.•Environmental Research Letters•2025

  • On the potential of Stommel’s perpetual salt fountain for artificial upwelling

    Open Access•Jost Kemper, Jan Mense et al.•Environmental Research Letters•2025

  • Direct cooling effect of artificial upwelling dominates over its marine carbon dioxide removal potential

    Open Access•Malte Jürchott, Andreas Oschlies et al.•Environmental Research Letters•2025

  • The RCP greenhouse gas concentrations and their extensions from 1765 to 2300

    Open Access•Malte Meinshausen, Steven J Smith et al.•Climatic Change•2011

  • Hierarchy of calibrated global models reveals improved distributions and fluxes of biogeochemical tracers in models with explicit representation of iron

    Open Access•Wanxuan Yao, Karin Kvale et al.•Environmental Research Letters•2019

Citations per year3
Citation span2025 - 2025 (1)
Highly citedNo

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Open DOIOpen Access
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