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• W2022063173 abstract "[1] An atmospheric general circulation model, coupled to a mixed layer ocean, is subjected to a broad range of forcing away from the current climate between 1/16 to 32 times current CO2 in halving/doubling steps. As climate warms climate sensitivity weakens (although not monotonically), albedo feedback weakens (driving much of the sensitivity weakening), water vapour feedback strengthens (at a rate slightly larger than it would if relative humidity remained unchanged), and lapse rate feedback increases (negatively); this latter change essentially offsetting the water vapour increases. Longwave cloud feedbacks are relatively stable (moderate and positive) across the full range; shortwave cloud feedback remains relatively weak, apart from under the coldest climates. Cloud optical property related components (from total water content, water/ice fraction and cloud thickness) remain remarkably stable. Cloud ‘amount’ feedbacks show the greatest trends: weakening as temperatures increase. Although cloud feedbacks show an overall consistency of features in different latitudes, precise patterns of changes differ substantially for different baseline climates." @default.
• W2022063173 created "2016-06-24" @default.
• W2022063173 creator A5026645501 @default.
• W2022063173 creator A5051346632 @default.
• W2022063173 date "2009-01-03" @default.
• W2022063173 modified "2023-10-05" @default.
• W2022063173 title "Climate feedbacks under a very broad range of forcing" @default.
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• W2022063173 doi "https://doi.org/10.1029/2008gl036268" @default.
• W2022063173 hasPublicationYear "2009" @default.
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