Fig. 3: OH, CH4 oxidation and O3 radiative forcing.
From: Chemistry-driven changes strongly influence climate forcing from vegetation emissions
Percentage change in OH in lowest 5 km for (a) Strat-Trop (STΔ) and (b) CRI-Strat 2 (CS2Δ). Zonal mean change in CH4 oxidation flux for (c) STΔ and (d) CS2Δ - STΔ. Forcing from O3 changes (SARFO3) for (e) STΔ and (f) CS2Δ, values in title show global mean forcing.
