Fig. 2: Radiative forcing, radiative efficiency (ϕ) and feedback factor (α) from a doubling of BVOC emissions in a pre-industrial (PI) atmosphere. | Nature Communications

Fig. 2: Radiative forcing, radiative efficiency (ϕ) and feedback factor (α) from a doubling of BVOC emissions in a pre-industrial (PI) atmosphere.

From: Chemistry-driven changes strongly influence climate forcing from vegetation emissions

Fig. 2

We show the individual forcing components from changes to O3 (SARFO3), CH4, the aerosol direct radiative effect (IRFDRE) and aerosol-cloud interactions (CRE) and their combined totals (Net) for Strat-Trop (STΔ) and CRI-Strat 2 (CS2Δ). The left axis shows the radiative forcing, the inner right axis the radiative efficiency and the outer right axis the feedback factor. Error bars show the standard error.

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