The liquid water path (LWP) adjustment due to aerosol–cloud interactions in marine
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates.
An unequivocal attribution of LWP adjustments to changes in aerosol concentration from
climatology remains difficult due to the considerable covariance between meteorological
conditions alongside changes in aerosol concentrations. We utilise the susceptibility
framework to quantify the potential change in LWP adjustment with boundary layer (BL) …

The liquid water path (LW P) adjustment due to aerosol-cloud interactions in marine
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates.
An unequivocal attribution of LW P adjustments to changes in aerosol concentration from
climatology remains difficult due to the considerable covariance between meteorological
conditions alongside changes in aerosol concentrations. We utilise the susceptibility
framework to quantify the potential change in LW P adjustment with boundary layer (BL) …