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. Author manuscript; available in PMC: 2020 Jul 23.
Published in final edited form as: J Clim. 2018 May 17;31(11):4429–4447. doi: 10.1175/JCLI-D-17-0439.1

Figure 3:

Figure 3:

Global (left) and regional (right) annual multi-model mean temperature change, precipitation change and apparent hydrological sensitivity (AHS) in the regional (SULASIA, SULEUR, BCASIA; performed by seven models) and global (SO4x5 and BCx10; performed by 9 models, from Samset et al. (2016)) experiments. The error bars represent ±1σ of the annual mean response across the models. The global AHS in BCASIA excludes the value from GISS (−104±1770 %/K) since it is very different from others, due to a too small global temperature response signal involved in the calculation (primarily caused by extreme cooling in the North Atlantic). The Asian AHS in BCASIA excludes the value from IPSL-CM5A (66±627 %/K) for the same reason.