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• W2185030261 abstract "Understanding cloud vertical structure is crucial for climate studies due to its impact on both the magnitude and sign of net cloud radiative forcing; for example, low thick clouds like boundary layer stratocumulus have a net cooling effect, but high thin clouds like cirrus have a net warming effect (e.g. Liou 1986; Hartmann et al. 1992). The vertical distribution of clouds also modifies both the latent and radiative heating profiles of the atmosphere and affects general circulation and moisture transport (Webster and Stephens 1984; Randall et al. 1989). In a climate simulation study, Wang and Rossow (1998) found that changing the cloud vertical distribution can significantly modify the strength of the Hadley circulation. In their two-layer cloud simulations, the strength is a strong function of the separation distance between the two cloud layers. Placing a single-layer cloud at a mid-level gives rise to the strongest Hadley circulation. So far, we have poor knowledge of cloud vertical distribution on large scales, which due mainly to a shortcoming in direct measurements. The current passive satellite observations provide the only means of obtaining the large-scale and global cloud information, but unfortunately many limitations exist in the conventional satellite cloud retrieval schemes." @default.
• W2185030261 created "2016-06-24" @default.
• W2185030261 creator A5014880079 @default.
• W2185030261 date "2005-01-01" @default.
• W2185030261 modified "2023-09-27" @default.
• W2185030261 title "A Comparison of the Global Surveys of High, Mid, and Low Clouds from Satellites and General Circulation Models" @default.
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