Fig. 6
From: The amplifying influence of increased ocean stratification on a future year without a summer
Responses in OHC with depth to the 1815 eruption. a Evolution of SW-Catm (left axis) and OHC (right axis) across various ocean layers. b Anomalies in zonal mean ocean temperature by depth and latitude in 1816, with stippled regions indicating a consistent sign of anomalies across at least 14 of the 18 (80%) ensemble members. Shading in a denotes the range of two standard errors. Years indicated on the abscissas begin at the corresponding tick marks
