Table 1.

Total aerosol radiative forcing decomposed into Twomey, liquid water path, and cloud fraction components using Eq. 3 from thousands of trajectories initialized over global oceanic areas from ${\mathrm{60}}^{○}$S to ${\mathrm{60}}^{○}$N averaged over eight meteorological $LTS$ regimes

Forcing (W/${\mathrm{m}}^2$)	Day 1	Day 2	Day 3
Twomey	$-0.34\pm 0.28$	$-0.42\pm 0.31$	$-0.61\pm 0.41$
Liquid water path	$-0.06\pm 0.03$	$+0.09\pm 0.05$	$-0.04\pm 0.06$
Cloud fraction	$-0.25\pm 0.08$	$-0.08\pm 0.03$	$-0.08\pm 0.03$
Total	$-0.66\pm 0.30$	$-0.42\pm 0.31$	$-0.76\pm 0.42$