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The top documents tagged [stratosphere cool]
Climate Models. 1-D Radiative convective models The atmosphere is divided into several (about 50) vertical layers. Each layer can either represent the
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Radiation Group 3: Manabe and Wetherald (1975) and Trenberth and Fasullo (2009) – What is the energy balance of the climate system? How is it altered by
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Climate Models
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Radiation • Group 3: Manabe and Wetherald (1975) and
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