Climate, the statistical description of weather including the probabilities for anomalies, changes continuously, since both the interaction among the climate system components (atmosphere, ocean, biosphere, cryosphere, and lithosphere) and the irradiance of the sun vary on all timescales up to billions of years. On timescales which are of most interest for mankind, i.e. up to centuries, major factors causing climate variability are: changing composition of the atmosphere; spectral solar irradiance variations; systematic changes of ocean-atmosphere-land interaction, if resulting in major changes of ocean circulation; volcanic eruptions injecting mass into the low latitude stratosphere (>20 km height); and land cover change modifying the surf...