Fig. 3
From: The amplifying influence of increased ocean stratification on a future year without a summer

Global mean-simulated responses to the 1815 eruption. Simulated anomalies relative to 1814 are shown in a global mean clear-sky shortwave flux through the atmosphere (SW-Catm), 2-m air temperature (T), and precipitation (P), and b SW-Catm, global mean TOA incoming net (R T), shortwave (SW), and outgoing longwave (LW) radiation. Shading denotes the range of two standard errors. Years indicated on the abscissas begin at the corresponding tick marks