This absence risks systematic underestimation of projected future warming and overestimation of remaining carbon budgets. Using the MAGICC climate model, we projected that WIE could add 0.2 °C–0.4 °C of warming by 2100 across scenarios, split roughly equally between carbon dioxide and methane, amplifying post-2020 anthropogenic warming by 20%–30%.
This absence risks systematic underestimation of projected future warming and overestimation of remaining carbon budgets.
Using the MAGICC climate model, we projected that WIE could add 0.2 °C–0.4 °C of warming by 2100 across scenarios, split roughly equally between carbon dioxide and methane, amplifying post-2020...
Combined emission sensitivity and climate response 1σ uncertainties are ±0.2 °C on the added warming and ±10%–30% on the warming amplification.
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This absence risks systematic underestimation of projected future warming and overestimation of remaining carbon budgets. Using the MAGICC climate model, we projected that WIE could add 0.2 °C–0.4 °C of warming by 2100 across scenarios, split roughly equally between carbon dioxide and methane, amplifying post-2020 anthropogenic warming by 20%–30%. Combined emission sensitivity and climate response 1σ uncertainties are ±0.2 °C on the added warming and ±10%–30% on the warming amplification.
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