Assesses climate outcomes of co-scaling carbon solutions, suggesting enhanced efficacy over single-pathway approaches.
by 2100, cuts the 1.5 °C overshoot duration by roughly half, and limits end-of-century warming to 1 °C rather than 1.37-1.39 °C. Relative to the recent focus on Decarb-Led pathways, Co-Scale's main constraints is the feasibility of geological carbon storage, while food, water, and cost pressures are comparatively less restrictive.
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Ampah et al. (2026) studied this question.
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