Titlebook: Climate Sensitivity to Radiative Perturbations; Physical Mechanisms Hervé Le Treut Conference proceedings 1996 Springer-Verlag Berlin Heid

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Water Vapour and Cloud Feedback in the BMRC AGCM integration of a model using the solar insolation for fixed season and fixed sea surface temperatures (SSTs) and sea ice. The SSTs are perturbed by a uniform amount (usually ± 2°C) about their appropriate climatological values (Alexander and Mobley, 1976). The top of atmosphere (TOA) changes in lon

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Cloud-Radiative Feedback as Produced by Different Parameterizations of Cloud Emissivity in CCM2(1990). This negative cloud feedback is due to enhanced longwave emission caused by reduction of high clouds in a warmer climate (Zhang et al., 1994). Since longwave emission from clouds is closely related with cloud emissivities, and there are large uncertainties in their parameterization in the up

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https://doi.org/10.1007/978-3-642-61053-0Cloud; Snow; atmospheric radiation; atmosph?rische Strahlung; climatology; global warming; globale Erw?rmu

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