Download Climate Sensitivity to Radiative Perturbations: Physical by Gerald L. Potter, Michael Fiorino (auth.), Hervé Le Treut PDF

By Gerald L. Potter, Michael Fiorino (auth.), Hervé Le Treut (eds.)

Current weather types diverge of their overview of world warming that might outcome from the anthropogenic bring up in hint gases. it's because they range of their illustration of the hydrological cycle (water vapour, clouds, snow and sea ice, soil moisture) and since an instantaneous validation by way of sensitivity isn't attainable. oblique tools and ways are as a result essential to make certain the types successfully. The e-book presents an outline on various validation ways. using satellite tv for pc information is especially stressed.

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Extra info for Climate Sensitivity to Radiative Perturbations: Physical Mechanisms and Their Validation

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Rowntree, 1990: A mass flux convection scheme with representation of 32 cloud ensemble characteristics and stability dependent closure. Mon. Wea. , 118, 1483-1506. , 1993: Parameterization of moist convection i the NCAR Community Climate Model (CCM2). Submitted to 1. Geophys. Res.. Kuo, H. , 1974: Further studies of the parameterization ofthe influence of cumulus convection on large-scale flow. 1. Atmos. , 31, 1232-1240. Manabe, S. and RE Strickler, 1964: Thermal equilibrium of the atmosphere with a convective adjustment.

1. E. ScWesinger, 1994: Analysis of global cloudiness: 2. Comparison of ground-based and sateIlite-based cloud c1imatologies. J. Geophys. , 99, in press. , 1994: A Summary Documentation of the AMIP Model. PCMDI Report No. 18. Program for Climate Model Diagnosis and Intercomparison, Lawrence Livermore National Laboratory, Livermore, CA, 343pp. ·Schiffer, 1991: ISCCP cloud data products. Bull. Amer. Meteor. , 72,2-21. G. Wellemeyer, EE Eck. Y,M. Yeh and the Nimbus-7 Cloud Data Processing Team, 1988: Nimbus-7 global cloud climatology.

The consideration of short time and spatial scales is a necessary step for such an evaluation because it makes it possible to inspect the different primary physical processes. In the tropics, this evaluation may concern many aspects of the model variability such as: the diurnal variation and the spatial organisation of the deep convective cloudiness; the characteristic time scale of the fluctuations in different regions and the interaction between convection and tropical disturbances (such as African Easterly waves or the Intraseasonal oscillation).

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