Extended Data Figure 3: Total changes and rapid adjustments for LvP and SWA.
From: An observational radiative constraint on hydrologic cycle intensification
a, The total change in LvP per unit warming (mean over years 131–150 of the abrupt4 × CO2 simulation minus the corresponding mean of the piControl simulation, normalized by 2-m air temperature change, LvΔP/ΔT) versus total change in clear-sky SWA per unit warming (clr-ΔSWA/ΔT). b, The rapid adjustment of LvP versus rapid adjustment of clear-sky (clr-) SWA. A linear fit is shown in both cases.
