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• W2051806239 startingPage "3019" @default.
• W2051806239 abstract "Abstract Anthropogenic forcings, such as greenhouse gases and aerosols, are starting to show their influence on the climate, as evidenced by a global warming trend observed in the past century. The weakening of tropical circulation, a consequence of global warming, has also been found in observations and in twenty-first-century climate model simulations. It is a common belief that this weakening of tropical circulation is associated with the fact that global-mean precipitation increases more slowly than water vapor. Here, a new mechanism is proposed for this robust change, which is determined by atmospheric stability associated with the depth of convection. Convection tends to extend higher in a warmer climate because of an uplifting of the tropopause. The higher the convection, the more stable the atmosphere. This leads to a weakening of tropical circulation." @default.
• W2051806239 created "2016-06-24" @default.
• W2051806239 creator A5002841093 @default.
• W2051806239 creator A5014112567 @default.
• W2051806239 date "2010-06-01" @default.
• W2051806239 modified "2023-09-23" @default.
• W2051806239 title "Depth of Convection and the Weakening of Tropical Circulation in Global Warming" @default.
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• W2051806239 doi "https://doi.org/10.1175/2010jcli3383.1" @default.
• W2051806239 hasPublicationYear "2010" @default.
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