GSTDTAP  > 气候变化
DOI10.1029/2021GL094948
Suppressed late-20th Century warming in CMIP6 models explained by forcing and feedbacks
Christopher J. Smith; Piers M. Forster
2021-09-13
发表期刊Geophysical Research Letters
出版年2021
英文摘要

For the 1960-2000 period, the latest generation of climate models (CMIP6) shows less global mean surface temperature change relative to pre-industrial than that seen in observations. In contrast, the previous generation of models (CMIP5) performed well over this period. It has been hypothesised that this suppressed late-20th Century warming seen in CMIP6 is caused by a stronger aerosol forcing. However, we find this to be only part of the story. Not only is the aerosol forcing marginally more negative in CMIP6 compared to CMIP5, the greenhouse gas forcing in CMIP6 is also weaker than in CMIP5. These forcing differences are amplified by differences in climate sensitivity between the CMIP5 and CMIP6 ensemble, which leads to both a stronger aerosol cooling over 1960–1990 and a stronger greenhouse gas induced warming from 1990, returning the warming post-2000 towards the observed level.

领域气候变化
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文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/338773
专题气候变化
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Christopher J. Smith,Piers M. Forster. Suppressed late-20th Century warming in CMIP6 models explained by forcing and feedbacks[J]. Geophysical Research Letters,2021.
APA Christopher J. Smith,&Piers M. Forster.(2021).Suppressed late-20th Century warming in CMIP6 models explained by forcing and feedbacks.Geophysical Research Letters.
MLA Christopher J. Smith,et al."Suppressed late-20th Century warming in CMIP6 models explained by forcing and feedbacks".Geophysical Research Letters (2021).
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