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

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Dedekinds Untersuchungen zum Zahlbegriff,. Thus, we have the opportunity to compare the sensitivity of these two models which were also used for time-slice 2*.. experiments (mahfouf et al., 1994a et Timbal et al., 1995). Since ARPEGE includes a wider range of options, we have performed three sets of experiments to study the impact of a new

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Conference proceedings 1996they differ in their representation of the hydrological cycle (water vapour, clouds, snow and sea ice, soil moisture) and because a direct validation in terms of sensitivity is not possible. Indirect methods and approaches are therefore necessary to verify the models efficiently. The book provides a

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https://doi.org/10.1007/978-1-349-12309-4ount error accounts for much of the error in short-wave cloud forcing because short-wave cloud forcing has a linear dependence on cloud amount. Some of the errors in short-wave cloud radiative forcing cannot be explained by errors in cloud amount and may be due to errors in cloud optical properties.

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AMIP Diagnostic Subproject on Cloud Forcing: Some Preliminary Findingsount error accounts for much of the error in short-wave cloud forcing because short-wave cloud forcing has a linear dependence on cloud amount. Some of the errors in short-wave cloud radiative forcing cannot be explained by errors in cloud amount and may be due to errors in cloud optical properties.

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https://doi.org/10.1007/978-1-349-12309-4unts to an underestimate in atmospheric SW absorption by more than 30 W m., a substantial discrepancy. This result implies that clouds absorbed more SW radiation than expected. There has been a long history of unexplained anomalous cloud absorption of uncertain magnitude (Stephens and Tsay, 1990).

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