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Climate
Cloud reflection 20%
Atmosphere Reflection 6%
Atmosphere and cloud radiation 64%
Earth surface reflection 4%
Direct earth radiation 6%
Solar energy 100%
Atmosphere absorption 16%
Atmosphere absorption 15%
Cloud absorption 3% Redirection and convection 7%
Land and water body absorption 51%
Latent heat 23 %
Fig. 1.6 The Earth’s radiation balance Solar radiation (yellow) warms the Earth’s atmosphere and the Earth’s surface, and is released as heat radiation (red). Part of the heat radiation is transmitted back to Earth by gases in the atmosphere, turning the atmosphere into a sort of natural greenhouse (according to NASA). Bereitgestellt von | De Gruyter / TCS Angemeldet | 212.87.45.97 Heruntergeladen am | 08.11.12 15:13