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Published byFelix Little Modified over 9 years ago
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Introduction to Climate and Environmental Physics HS 2014 Lecture II Christoph Raible, Markus Leuenberger, Fortunat Joos and Thomas Stocker
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Normalised λ E λ
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340-100 = 240 161+79 = 240 397-342+20+85+79 = 239
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Top of atmosphere (TOA) Net Short Wave (W/m2)
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Top of atmosphere (TOA) Net Long wave (W/m2)Net total (W/m2)
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At the surface Net short wave (W/m2)Net Long wave (W/m2) Net total (W/m2)
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Sensible heat flux (W/m2)Latent heat flux (W/m2)
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Global warming GHG concentrations in the atmosphere trap the long wave outgoing radiation of the surface There is a fast feedback of a warming atmosphere on its water vapor content Feedback of the surface albedo, e.g. sea ice, deforestation, … Aerosol concentrations lead to scattering and absorption of incoming radiation and affects the cloud building process Natural changes, e.g., solar activity, volcanos, orbital parameters
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