Marine carbon sink after temperature overshoot is dominated by biological pump carbon

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Michael Hayes

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Feb 12, 2024, 7:25:21 PM2/12/24
to Carbon Dioxide Removal
[...] Net removal of CO2 from the atmosphere may be required to reach the Paris Agreement 
goals to limit warming well below 2°C. Under such ‘net-negative-emissions’, the relative role 
of different marine processes in storing additional CO2 remains unknown. Here we use 
idealized Earth System model experiments to understand the response of different marine 
carbon uptake and storage mechanisms under a range of idealized emission scenarios. We 
find that the physical-chemical mechanisms, generally known to dominate under increasing 
CO2-emission, contribute little to additional CO2 storage after CO2 or temperature overshoot. 
Biological-carbon storage emerges as an increasingly and eventually dominating carbon-
storing mechanisms on multi-centennial timescales. Understanding how the ocean responds 
to complex emission trajectories is essential to guide science-based solutions to the climate crises.[...]

https://scholar.google.com/scholar_url?url=https://www.researchsquare.com/article/rs-3921898/latest.pdf&hl=en&sa=X&d=16114824898549127898&ei=_X3KZaWeOujSy9YP4am1oAs&scisig=AFWwaeaNuMjRSbDTEwtTnBVI2pLO&oi=scholaralrt&hist=Mp0zpXoAAAAJ:1263629159855157386:AFWwaea3IolKxz2qNiREQneorIKq&html=&pos=6&folt=kw 

MH] Oceanic Farming is likely more of a CDR need than just another mCDR option. 

Michael Hayes

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Feb 13, 2024, 1:30:23 PM2/13/24
to Carbon Dioxide Removal
[...] With potentially delayed CO2-mitigation efforts, net-negative CO2-emissions may be required 
to return to acceptable limits of climate warming as defined by the Paris Agreement. The 
ocean is an important CO2 sink under increasing atmospheric pCO2, when physico-chemical 
CO2-uptake dominates. The processes that govern its role under net-negative CO2-emission 
regimes are, however, unclear. Here we assess changes in marine CO2-uptake and storage 
mechanisms under a range of idealized temperature-overshoot scenarios in an Earth System 
model of intermediate complexity over centennial timescales. We show that while the fate 
of CO2 from physical-chemical uptake is very sensitive to future atmospheric boundary 
conditions, storage associated with the biological carbon pump continues to increase and 
may even dominate marine excess CO2 storage on multi-centennial time scales. Since change 
in biological pump carbon is strongly linked to the oxygenation status of the ocean, 
improved prediction of marine deoxygenation turns out to be a key to better forecast the
future of the marine carbon sink on multi-centennial time scales.[...]
MH] Improvements in Oceanic Farming technologies should be able to take advantage of this longterm trend. 

Michael Hayes

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Feb 14, 2024, 4:03:04 PM2/14/24
to Carbon Dioxide Removal
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