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

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https://doi.org/10.1007/978-3-642-67184-5, on the cloud generation scheme, and on details of the treatment of the cloud-radiation interactions (overlap assmption, representation of mixed phase clouds). We conclude that, although the ECMWF prognostic cloud scheme is more physically based and gives better representation of clouds and related

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https://doi.org/10.1007/978-3-662-68142-8 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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Dedekinds Untersuchungen zum Zahlbegriff,exploring this subject, are the 3-D General Circulation Models (GCM). The response to an increase in greenhouse gases have shown many differences between models (Schlesinger and Mitchell, 1987).The sensitivity to external forcing is a key parameter of the response of the CGM. Cess and Potter (1988)

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,Modelli di percorsi Cammini con capacità,This paper reviews the role of water vapor in climate sensitivity, the factors determining water vapor concentrations, comparisons of observed and model behavior of water vapor, and indirect and direct approaches to determining the actual climate feedback.

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Evaluation of the Spatio-Temporal Variability of Tropical Convection in GCMs by Using Geostationary ained from a comparison between the ECMWF model and Meteosat data over Africa and the Atlantic Ocean. Three model time series are used based either on “first guess” or on two runs without assimilation. The aim of the “first guess” time series is to validate the response of the cloud parameterization