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Asian Anthropogenic Aerosol Forcing Played a Key Role in the Multidecadal Increase in Australian Summer Monsoon Rainfall


Fig. A1.

Spatial distribution of trends over 1930–2014 for DJF (a),(d),(g) precipitation, (b),(e),(h) sea surface temperature after removing the tropical mean trend (25°N–25°S), and (c),(f),(i) mean sea level pressure (color) with 850-hPa winds (vectors) in the (left) CESM2-All SMBB (40 ensembles), (center) CESM2-GHG (15 ensembles), and (right) CESM2-AER (20 ensembles) simulations from CESM2 Large Ensemble. Stippling shows regions where at least 70% of the ensemble members agree on the sign of change.

Citation: Journal of Climate 37, 3; 10.1175/JCLI-D-23-0313.1



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