Fig. 3: Direct and delayed response to tropical eruptions in CMIP6 models.
From: Extreme Tibetan Plateau cooling caused by tropical volcanism
a Composite SAT anomaly (shading; K) and 200 hPa geopotential height anomaly (contour; m) with respect to the five preceding years during the first boreal winter after 1982 and 1991 eruptions for the MME of historical runs. Stippling indicates temperature anomalies significant at the 95% confidence level. Solid and dashed contours denote positive and negative anomalies, respectively, and contour interval is 10 m. Purple lines corver the TP with altitude above 2500 m. The averaged SAT anomalies over the TP are listed in the upper right corner. b Same as (a) except for the AMIP runs.
